53D16NE8ee4 63.4856 BORLAND LAKE 010

GEOPHYSICAL INVESTIGATIONS

AT BORLAND LAKE, FAVOURABLE LAKE AREA,

RED LAKE MINING DIVISION, ONTARIO.

for

MASSIVE ENERGY LIMITED

by

J. B. Boniwell

Exploration Geophysical Consultant May 21, 1986

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L53D16NE0004 63.4856 BORLAND LAKE

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LIST OF CONTENTS

Introduction

Details of Survey

Data Presentation

Discussion of Results - A,

B,

C,

D,

IP/ResistivityMagneticsV.L.F. (radio) Em.Airborne Geophysics

Mineral Considerations

Conclusions and Recommendations

DV/G. NO.

EIC-16??-16?8

-16?9A,B-1680A.B

-1681A.B

-1682A.B

LIST OF DRAWINGS

TITLE

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24

58

121315

. 20

010C

Locality Plan Showing Grid Area

Elements of Structure, Airborne Data

Chargeability Contours, Gradient Array

Resistivity Contours, Gradient Array

Magnetic Contours

Plan of Interpretation

SCALE

1:253,440

1:10,000

1:1200

li 1200

1:1200

1:1200

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INTRODUCTION

A drilled mineralization rich in silver has been found to underlie parts of Borland Lake, about 250 kms. north of the town of Red Lake in northwestern Ontario. The mineral system is patently shear-controlled, and locally involves a number of irregular lenses of variable widths and grades. Strong lateral off-sets are evident in at least two localities. These conditions have rendered the task of adequately sampling the system awkward, but what has proven most difficult is the establishment of new extensions and repetitions.

Thus as an aid to on-going investigations, a programme of geophysics has recently been completed in the environment incorporating both lake and landward sections of the most prospective ground. This surveying has resorted to a combination of detailed magnetics and gradient array induced polarization (IP) applied systematically to supply a sought-after perspective.

The results obtained from this work form the basis of this reporting. They are however evaluated in conjunction with pertinent airborne data and some prior ground V.L.F. surveying in the area.

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STOUT LAKE

DEER LAKE

Scale l ^ 20 miles

930

FINGER LAKE

FAVOURABLE LAKE

930

SANDY LAKE

Scale l - 4 miles

1985Airborne Survey

Area

Geophysical Grid Area

REDLAKE

BUSH PILOT CORPORATION

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO

LOCALITY PLAN showing grid area

Dwg. No. E.I.C.-I677

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DETAILS OF SURVEY

The grid lines prepared for this fresh coverage were laid

out due N-S at intervals of 50' and 100', The controlling E-W

base-line passed through the heart of the mineral system as it is

presently known.

The desired magnetic survey was completed with a Gem

Systems GSM-8 proton precession magnetomer providing measures of

the total terrestrial field to a sensitivity of l nT.- A reading

accuracy of about 3 nT has been achieved through the

contemporaneous on-site use of a fixed self-recording base

station magnetometer, Canadian Mining Geophysics MR-10,

monitoring geomagnetic field change every l min. during the

currency of the field work.

The IP coverage was carried out by gradient array

requiring the grounding of current electrode pairs at distant

sites approximately 3000' to either side beyond the limits of the

grid in the traverse direction. This is the so-called normal

mode of operation for the array. Up to l? lines 100' apart, were

surveyed from one current dipole set-up, and a further 18 from a

second. A total of 3400' in the BL direction were so covered.

Time domain equipment was employed for this operation,

specifically a Phoenix Geophysics IT-1 transmitter providing a

rated 3.0 kw of power working in conjunction with a Huntec Mk IV

receiver which yielded up to 9 channels of decay time

information. The measuring dipole spacing was kept at 100'

throughout the traversing, observations generally taken every

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100' on line but were closed up in the immediate vicinity of the

.•showing to 50' .

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LDATA PRESENTATION

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The collected data after suitable computation and

correction have been posted in plan and contoured. The plan

scale throughout is 111200.

Three parameters have been presented, viz. total field magnetics, apparent chargeability and apparent resistivity. The contour intervals vary for each, from 10 nT up to 1000 nT for the

magnetics, 0.5 millisec for the chargeability and 100 to 1000 ohm-metres for the resistivity. Contouring has been undertaken

by hand for all three parameters.

Features brought out by the subsequent interpretation of these results have been compiled into a suitable overlay.

As part of the current evaluation, consideration has been

given to the airborne geophysical results which were recorded in an earlier surveying of the region. These data included

magnetics, V.L.F. (radio) em. and conventional frequency em. measurements collected by low level helicopter flying under the

guidance of (Mini-Ranger) electronic navigation. The chief interpreted elements of structure and lithology perceived

therein, which pertain to the present ground search area, have

been compiled at a scale of 1:10,000. This hews to the base scale of all the air-data presentations and thus allows

correlations therewith.

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DISCUSSION OF RESULTS

L A. IP/Resistivity (Dwg. Nos. EIC-16?9, 1680)

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These results are accorded priority since they are likely

to reflect most directly the mineralization itself. A singular

showing (the Johnston showing) at the lake edge offers a valuable

control.

Thus it is promising that at the western shore of Borland

Lake where this best exposure exists, a recognizable

chargeability anomaly has been obtained in correlation. In

amplitude terms, it is quite a modest response, two and a half

times background at best, but it is unmistakable. It is

constrained in size, and is also accompanied by a heightened

resistivity locally which implies an attendant silicification.

All this fits well the manner and style of the mineralization as

it has been revealed and defined by drilling.

It is therefore remarkable, and of extreme pertinence to

exploration prospects in the area, that this anomaly does not

behave in a predictable fashion. While to the east there is a

discernible tail extending out into the lake broadly on strike,

there is nothing comparable to the west. Instead, the anomaly

there swings sharply to the south-west, and stays on this course

for nearly 300' before petering out. That this is no weird

aberration of data is confirmed by the resistivity results which

behave even more pronouncedly in the same manner. It appears

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probable therefore that the mineral zone has been warped in this

way under the influence of cross-structure,

Once this concept is accepted, several possibilities open

up. The responsible structure here is projected to be a NE fault

which lies just off-shore, and so has been hidden from past

conventional mapping. It also seems to have escaped drilling!

certainly it has not been tested in any section where the results

would be telling and umambiguous. Importantly, this cross-fault

intersects the known vein system where the best mineralization

appears to be concentrated j for example, the intercept obtained

in DDK #65-2 wherein an average 12.5 ozs. Ag over 109,4' (33-35

m) was recorded occurs in the vicinity, and it is the premier

intersection of the drilling so far. Since immediately adjacent

holes failed significantly to match this intersection, the

inference can be drawn that the main zone has indeed swung off

the drill grid, or has been locally interrupted.

Potentially then cross-structures form a critical part of

the mineral setting in this environment. This likelihood however

may not make exploration any easier. It implies instead that

rather than one coherent mineralized system, there will be a

number' of broken up bodies., possibly of different ages, and

occupying a variety of positions and attitudes.

This indeed appears the case. Further afield on the

grid, such polarization anomaly that has been obtained occurs in

a scatter. There is no strong sense of a governing throughgoing

system. Nonetheless several of these individual events are -in-

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triguing in themselves. Manifestly the most notable, -- it being

one of the strongest polarization features of the survey has been encountered on lines 15W, 16W as they straddle the edge of

Solon Pond. The high positive centre is flanked by some equally

low troughs, and the indication is that current flow threading

this sector has been radically distorted by contravening current

paths. The effects are typically local and pronounced. It is

considered most probable that cross-faulting has wrought at least

part of this disorder, although the strike bearings of the axes

involved are not immediately evident. Resistivities tend to be

unhelpful in this regard as they drop environmentally to extreme

lows. In all, this is a very remarkable locality, and its

significance is more specifically addressed in a later sector.

Among other chargeability features of the area is a zone

of high which emerges from Borland Lake at 500S/2000N in the

southern quarter of the area. It is accompanied by lowered

resistivities and although in part due to the lake itself, this

is a characterizing condition that se'ts it apart from the

Johnston mineralization. It is also an incomplete anomaly,

remaining open to the east.

To the north-east of the showing sector, a complex Of IP anomaly has been obtained} in fact all across the northern

reaches of the grid, a sprawl of anomaly exists, much of it

untidy and locally irregular. Several sources are presumed

present, some of them ostensibly formationally controlled, others by structure. High resistivity correspondence appears in two

places, viz. at 650N/300E and at 1250E/1900W} and in both .

instances outcrop is present. It follows these rocks should be

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closely examined and sampled, both for their chargeability propensities and their mineral content, particularly in the first location where considerable shearing and carbonitization have been mapped in felsic volcanics.

In this general vicinity, the evidence that structure is also contributing to anomaly distribution is chiefly supplied by the lobe of chargeability response which extends SW towards the Johnston showing. It does not quite reach that far but its on-strike affinity with the arm which does extend south-west beyond there is unmistakable. Increasingly it appears that this particular axis forms part of the mineral history of the

environment, albeit in this latest section resistivities do not

climb typically, but drop off, presumably in part because of the effects of the lake. Moreover in this neighbourhood there appear again some strange peak IP highs and lows which, although much more confined, hark back to the Solon Pond situation. Since transgressing structure is strongly suspected in that first case, so ought it be here in the second.

Again therefore this is an interesting locality with more

than one facet to consider and sample.

B. Magnetics (Dwg. No. EIC-1681)

Dramatically, the main drilled mineralization provides an anomalous trace in the obtained magnetics.. This was not expected. The expressions involved amount to 400 nT in local

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relief, and their correlation with the mineral system is faithful and undeniable. An ultramafic finger, presumably a sill, approximately 6' wide, appears in the drilling about 200' to the south side of this argentiferous zone, and is potentially a factor, but where fair comparisons can be made, it is not a major one. It seems that there is enough pyrrhotite extant in the mineral assemblage to account for most of the observed effects here.

ii_

Whether this association represents a general condition for the area however suddenly becomes a crucial question, for it is evident that the zone of magnetic anomaly does not extend in any strength beyond the limits of past drilling. Even more disconcerting, it does not follow the IP through its apparent curve to the south-west across lines 200W et al. At issue is whether the magnetics are more accurately reflecting the important mineral incidences of the area, or whether the IP results are.

If it is the magnetics, then it is clear not too much more can be anticipated from the on-strike possibilities of the main zone. Some weak anomaly across lines 700W-900W, and a couple of very confined, semi-isolated peaks positioned around the edges of Solon Pond virtually represent the entire potential for new occurrence to the west. Despite their strength, there is little encouragement inherent to either of the latter events. To the east, it is possible to suppose extra extension as the zone closely approaches the peridotite intrusion in the lake, on the assumption that all magnetic definition of it is lost to the overwhelming influence of the ultramafic. But this of course is

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largely speculative, notwithstanding the hints in drilling of mineralization on the intrusive (south) flank. More to the point is the clear indication that magnetic anomaly does not conform to the principal IP/resistivity ridge which extends eastwards from the Johnston showing. This circumstance implies that the magnetics in following the known mineralization is tracing in effect the locus of the host shear; the IP/resistivity alignment (heading due east) must thus be describing a separate system, whether formationally or structurally controlled.

It therefore becomes important at this stage to look' at the other features the magnetics supply. There are two other zones of anomalous high. One in the northern parts of the grid, circa 900N, lines 500E-200E, denotes the presence of an iron formation according to outcrop evidence. This is neither a large system nor a strong one, but it implies a bedded unit relatively rich in magnetite. As such, it promises a useful marker for the environment. Unfortunately, it is neither very extensive here it quickly strikes off the grid -- nor is it distinctly a chargeability.

Across the south-west corner of the grid, a stronger, more compound magnetic system appears. It too follows a broad WNW orientation, and in consequence it might also be formational in origin, However in this instance, there are far more irregular components present. As a result, the system could indicate a string of several ultramafic pods, or more evocatively, a broken up sill of similar material potentially disposed about a synclinal fold. Small outcrops of peridotite appearing where the system crosses the shorelines of Borland Lake

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and Solon Pond reinforce the source probability at least.

To the west of Solon Pond, a broad high of magnetics

supposes that another large ultramafic intrusion occurs there,

again in a locality of little or no outcrop. This feature

remains open to the west, and according to the aeromagnetics

extends for approximately another 1500'.

Given all these intimations of ultramafic intrusion in

the grid area, the weight of evidence suggests that, of the two,

the IP data are more indicative of sulphide mineralization in the

environment than the magnetics. This of course is not too

surprising a 'conclusion, but it can not be taken very far since

-- inevitably it seems -- there is always some polarization

associated with the ultramafics, and some of this response is

undoubtedly due to magnetite. Still the hope remains that there

exist interesting sulphides in the area which contain no

pyrrhotite or magnetites and it is these sulphides which loom as

the new targets for exploration if mineral potential is to be

materially increased here.

Beyond these considerations, the magnetics do not reveal

much in the way of background geology, due. largely to the lack of

contrast across the bedded lithologies. The further fresh

insights to be obtained are all structural in connotation, and

these are evaluated in conjunction with other data, especially

including the V.L.F. em.

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C. V.L.F. (radio) Em.

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Some earlier acquired ground V.L.F. em. data (1985) can

be usefully integrated into present considerations. Although

coverage is more limited than both the magnetics and IP, and was

effected on a differing grid from one transmitter station only

(NAA, Cutler, Maine, broadcasting at 24.0 kHz), there are some

anomaly features which merit note.

The pre-eminent results in the current context is the

anomaly expression which has been obtained in direct correlation

with the showing mineralization. This correspondence, so far as

the coverage allows, starts and ends with the main zone as

defined by drilling. Thus V.L.F. surveying confirms what the

magnetics have already implied: further on-strike extensions of

the silver zone appear limited.

Yet there is evident considerable V.L.F. anomaly aligned

in sub-parallel systems. Several of these might be ascribed to

lithologic boundaries within the formational sequence, that is,

they are run-of-the-country events, but most are likely due to

shears'. For example, a good case can be made for the anomaly

axis which borders the north shore of Borland Lake since shears

in felsic volcanics have been mapped locally here. However what

remains most of interest to present considerations is the

indication of cross-structure in these data.

Unhelpfully, the lines of the V.L.F. grid run virtually

in the same direction as the critical, most strongly postulated

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cross-faulting, that is NE-SW. Resolutions in consequence are

very poor. Just the same, some clues to such faulting do reside

in the (contoured) results. In addition there is indication from

place to place of N and NW faults. Their significance is

unknown.

Taking all the signs of cross-structure together,

absorbing as well those furnished by the airborne geophysics, the

fault axes which appear most realistic to the area are as shown

(Dwg. No. EIC-1682). As can be seen, the NE-SW set appears to

dominates these faults find support in all methods. Only the

shears, or strike faults have a stronger combination of

expression, partly because they are more frequent, and partly

because they have been favoured by the grid (and flight path)

orientation.

D. Airborne Geophysics

In 1985, Aerodat Ltd. were contracted to overfly the

Borland Lake sector as part of a wider coverage. Besides

magnetics and V.L.F., measurements were collected with conventional em. (operating frequencies 9^6 Hz, 4575 Hz).

However no em, anomaly was recorded within the present grid area.

The magnetic and V.L.F. results on the other hand provide

evidence of anomaly trends which cross the area at a scale that

is regional in scope. Thus the mineral zone is largely not seen

for itself in either data set, although the magnetic ridge across

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the Johnston showing point does make itself evident; nevertheless

in this presentation it appears confusingly as a westward poking

tongue merely of the ultramafic intrusion in the lake whose

anomaly commands this locale.

As to be expected, the skein of ultramafic bodies in the

south of the grid area appears as a more homogeneous whole in the

air-data, and as already noted, more extensive. While these

kinds of melding do not aid the present interpretation

particularly, overall they do supply some sort of perspective.

Thus the larger regional faults can be seen with more clarity at

this scale than at the grid scale, and it is in this regard, the

airborne data make fair contribution.

As foretold, the strongest cross-breaks occur on the

NE-SE orientations there appears a family of them in the region.

But really for the first time, structures with N-S headings

become manifest. One of them passes through Solon Pond, and as

will be implied, this could be important to future mineral

chances.

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MINERAL CONSIDERATIONS

To begin with outcrop, the showing mineralization at the lake edge has provided geophysical responses in chargeability, resistivity, magnetics and V.L.F. em., all in fair coincidence. It would appear therefrom that projections of new occurrence ought to be straightforward. However in fact, they have proven far from simple.

This is because outside this one locality, there is no repetition of such a convergence of geophysical events anywhere else in the area, even along the immediate strike of the mineral zone as it has been outlined by drilling. It appears in consequence there are a number of divergent factors controlling mineralization in this sector, not all of which have previously been recognized.

Tackling the most logical possibilities first, viz. the on-strike extensions of the WNW fracture system passing through the showing setting, it is suggested by correlating resistivity and magnetic highs that this axis weakly reappears after an interceding break to pass through 250N/700W going on to 350N/900W. Over the relatively short 300' strike distance involved, there is exhibited a combination of modest magnetic and resistivity high, and it seems fair to add it to the strike extent of the showing system, especially since there is a weak companion IP anomaly at the east end. However there is no persistence, and V.L.F. tends to veer away southwards to pass it by. Moreover, a drill hole, #65-23, appears to have already

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probed this weak feature, presumably without notable success.

To the east of the showing out into Borland Lake, the V.L.F, and magnetic correlations are maintained on strike, but disconcertingly, both the mainstream resistivity and polarization anomalies quickly diverge from the known mineralization, and in consort hew to an independent (due east) course. On closer examination, it can be seen that a weak tail of IP and resistivity high does in fact stay with the drilled mineraliza tion in its ESE extension, but that in the circumstances it is having difficulty making itself discernible.

All this means that there is much more contributing to geophysical anomaly in the area than the known silver zone. It follows that there is an urgent need to understand and identify these other components since they patently impinge on any widened mineral possibilities inherent to the geology of the environment,

There are two immediate targets to concentrate on. One is the strongly developed arm of resistivity and polarization anomaly which strikes SW from out of the showing setting. There is some V.L.P. evidence to suppose that this is a cross-structural fault alignment, and the attendant IP/resistivity responses suggest in consequence that some of the silicic mineral fluids in the silver fracture system have at the time of their incursion taken advantage of this intersecting line of weakness. However there is no comparable magnetic high in correlation; if anything, this zone is distinguished by a slight lowering of magnetic level locally. This infers an absence of pyrrhotite and of ultramafic intrusion both; and that fact may

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well signify that there are two kinds of mineralization and two

ages of veining present and threading the area.

If so, this second generation of occurrence has not been drilled, or for that matter sampled in any diagnostic way. There is no perceived reason why it should not carry precious metals, and that possibility alone is warrant enough to undertake its

early testing.

From this widened point of view, it appears of some moment that much of the IP anomaly recorded in the areas has a NE-SW bias at the same time as it attempts to follow E to ESE formational trends. The second target of priority interest embodies this twin influence but with a twist: the polarization axis appears almost N-S while the resistivity trends of the locale are almost E-W. The anomaly in question centres upon 600N/1600W on the edge of Solon Pond. The polarization involved nearly reaches ?0 msec., or that is more than twice that of the showing anomalyj moreover it is accompanied, not by a resistivity high, but by a vast low which drops to an extraordinary level of 2? ohm-metres and less locally. Even the latter however is not confined to the chargeability but embraces an area roughly ?00' x 500' within a bay of Solon Pond. At the same time, there have been recorded within this realm some very large chargeability negatives adjacent to the positives. These infer, not inductive effects per se, but current reversals due to rather unusual body geometries and/or source dispositions. The very low resistivities themselves are believed primarily due to a clay which must come virtually to surface in places within.

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There is a lot to be explained here. The whole of this bay in one way or another is anomalous. Aside from the magnetics which are expressionless, the surrounding geophysics reiterates

the exceptional character of this locality. Nor is the behaviour of anomaly anything to do with the lake itself. That is evident just from the localization that has taken place within it. There

is too the sense of a centre, with bands of IP effects curving around it. The V.L.F. coverage unhappily is very skimpy right in

this section, but what results do exist demonstrate that strong

anomaly surely underlies this bay.

The most favoured interpretation of these remarkable

circumstances is a clay alteration product that has been

developed in a locality of great structural interaction. One

important aspect of this Solon Pond clay deposit is that it lies directly on strike with the (Johnston) silver zone fracture

system. Also it seems highly probable that a N, or NE bearing fault has intersected it here. The quasi-circular outline of the

bay, even, evokes images of a vent, that is, a brecccia pipe, raking NNE, perhaps in-filled by a (felsic) intrusive plug coming up it to near-surface. Whether this is a valid premise remains to be seen} also whether such a pipe would form a primary source to the silver mineralization likewise is unknown. But it is clear that there are discrete finite sources of polarization potentially due to metallics in this unique setting which beg to

be investigated.

What is learned here can then be transferred to two

lesser possibilities which unexpectedly exist to the ENE. In IP

terms there are similarities, the strong sharp highs for

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instance, and the rapid drop in resistivities, even a small negative polarization in one place, but the scale differs and there is no one centre. As before, intersecting fault structures are present, also as before, the magnetics are indifferent, but this time there is much more polarization about, and a fissure-type mineral emplacement seems more appropriate in consequence. There is no question this sector is interesting, and it too deserves follow-up, but more for itself than a stretched analogy with the Solon Pond events.

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CONCLUSIONS AND RECOMMENDATIONS

Some very intriguing results have been obtained by the combined geophysical surveying recently completed. They have also provided several surprises which will require eventual reconcilation with geplogy and the mineral probabilities of the area.

As things stand, the known silver mineralization has little conventional strike potential beyond the limits of drilling according to geophysics. A weak 300' extension across lines ?OOW and 900W is about all that can be forecast.

However, there are much wider possibilities for mineral occurrence in the area if several of the non-analogous, non-conforming anomaly features obtained in survey are ever found to represent emplacements of significant precious metal mineralization. Specifically there has emerged evidence severally of mineralized cross-structures, of bedded sulphidic horizons, and most unusually, of vents containing metallics. The most outstanding of the latter occurs in the pronounced north eastern bay of Solon Pond, most apparently affecting the shape . and style of this physiographic feature and surrounding terrain.

It is judged that at least three of these "outside" possibilities ought be subjected to intensive investigation, including drilling, in the next stage of exploration.

Increasingly i-t appears that the whole of the grid area constitutes an unusual mineralized environment, conspicuously

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spearheaded by the argentite mineralization of the Johnston zone.

There is much to learn here, and it is believed there are new and exciting prospects in the area that have yet to be discovered.

It is therefore recommended that the following steps be

undertaken}

i) all available drill core from past drilling on the silver zone be logged systematically by magnetic

susceptibility meter, and appropriate down-hole

profiles plotted;

ii) all other evidence of sulphides in the same core be

noted and plotted on section and in planj

iii) these data be reconciled with present geophysics!

iv) the rock outcroppings in the vicnity of 650N/300E,

and around 1250N/1900W be examined and sampled

geochemically for precious metal indication. In the

latter locality, the so-called Solon No. l Zone

prospect needs to be fixed with respect to the

present.grid j

v) on the basis of findings, a programme of diamond

drilling be embarked upon, the holes testing within

the showing environment and along its structural

strike such possibilities supported by geophysics

and seemingly not previously sampled adequately.

This could include the evident system extension

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vii)

viii)

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across lines 700W-900W.

notwithstanding any of the foregoing, the Solon Pond breccia pipe concept be drill-tested on its own merits. A suitable hole for the purpose would be i

DDK #86-Glt Collar at 750N/1400W

to be drilled grid SW at -50 for 450'

as for vi) above, a hole be drilled into the noted IP/resistivity zone branching south-west from the main (Johnston) showing location. Again a suitable

hole would be i

DDK #86-G2: Collar at 100N/300W

to be drilled grid SE at -50 for 350'

the complex of apparently structurally controlled IP

anomaly to the grid north-east be drilled as part of

the widened search for new mineral occurrence in the

area. An appropriate hole would be i

DDK #86-031 Collar at 600N/00to be drilled grid S at -50 for 450'

consideration be given to extending a complete V.L.F,

coverage to the present grid area. It ought be

possible to obtain concurrently on these lines

measurements in both the broadcast fields of NLK

(24.8 kHz), Seattle, Washington, and NSS (21\4 kHz),

t BXGAblBUR INTERNATIONAL CONSULTANTS LTD.

- 23 -

Annapolis, Maryland, to the considerable benefit of the overall programme.

x) future IP surveying be planned if the proposed tests prove encouraging.

The above cited drilling totals 1250'. This footage provides a reasonable minimum to initiate a test programme in the area, especially since all targets in each case represent potentially a new mode of occurrence. The holes are all collared on land to permit summer drilling if desired.

Finally it is concluded that if these recommendations are adopted, then a much better idea of the overall mineral potential of the environment will ensue. Besides that, the very testing herein provided may well furnish direct evidence of other important mineralization beyond the known silver zone, This eventuality, if it comes to pass, would of course open up a spate of new possibility, not just for jUhe 'immediate search area, but for the region as a whole.

May 21', 1986. J. B. BoniwellExploration Geophysical Consultant

BXGAblBUR INTERNATIONAL CONSULTANTS bTI).

53D16NE80a4 S3.4856 BORLAND LAKE

REPORT ON THE

1986 DIAMOND DRILL PROGRAM

AT THE

BORLAND LAKE PROPERTY

FOR

MASSIVE ENERGY LIMITED

SEPTEMBER l, 1986 Toronto, Ontario

Kenneth W. Johnson Project Geologist

53D16NE80M 63.4856 BORLAND LAKE020C

LIST OF CONTENTS

Introduction Page l

Property Location and Description l

Description of the Diamond Drill Program 5

Geology of the Borland Lake Deposit 5

Results of the 1986 Diamond Drill Program 6

Conclusions and Recommendations 7

Recommended Program and Proposed Budget 7

Appendix: Diamond Drill Reports No.'s 86-1 to 86-6 10

LIST OF DRAWINGS

Figure l

Figure 2

Figure 3

Figure 4

Figure 5

Property Location Map

Property Map - Borland Lake Area

Grade Thickness ContoursBorland Lake Deposit

3

4

Map Pocket

Plan of Diamond Drilling Map Pocket (l inch = 100 feet; E S. W sheets)

Longitudinal Sections showing Tonnage Map Pocket Blocks (i inch = 40 feet)

-2-

STAKED CLAIMS

KRL 697239 - KRL 697291 inclusive KRL 775009 - KRL 775043 inclusive

PIC LAKE AREA

53 claims 35 claims

Total Staked Claims 88

TOTAL NUMBER OF CLAIMS 98

At the present time Title to the above 98 claims is held by Noranda Exploration Co. Ltd. Under the terms of a Joint-Venture Agreement with Noranda dated February l, 1986, Massive Energy Ltd has earned a 59.8476% interest in the property through the expenditure of $216,029.95 on exploration during the period February l, 1986 to August l, 1986 (Massive Energy Ltd, unaudited statement, August l, 1986).

The following claims staked in 1984 and 1985 are held outright by Massive Energy Ltd. They were staked in order to cover the favourable geological formations between the Borland Lake and the Pic Lake claim groups.

28 claims43 claims41 claims3 claims6 claims2 claims2 claims2 claims4 claims4 claims3 claims

26 claims8 claims

KRLKRLKRLKRLKRLKRLKRLKRLKRLKRLKRLKRLKRL

793882823497823547823590823595823607823615823623823649823657823665823671828199

- KRL- KRL- KRL- KRL- KRL

KRL- KRL- KRL- KRL- KRL- KRL- KRL- KRL

793909823539823587823592823600823608823616823624823652823660823667823696828206

inclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusiveinclusive

TOTAL STAKED CLAIMS 172 Claims

Massive's 1986 diamond drill program concentrated on the Borland Lake silver deposit which lies within claims KRL 49061 and 49065.

x x

l /GODS'LAKE

MANITOBA s-3-

HUDSON BAY

V ONTARIO

.LINGMAN LAKE

BORLAND LAKE

Red * Lake

kenora

MUSKEGSAGAGEN LAKE

Thunder Bay-

PANGIS

USA

Timmins/)

^Sault Ste. Marie

QUE BEC

CASA BERARDI Matagami

Val d 'Or

Ci'rklqnd l Lake

Toronto

MASSIVE ENERGY LTD

LOCATION MAP

BORLAND LAKE PROPERTY

INTRODUCTION

In May 1986, Massive Energy Limited completed a limited diamond drill program on the Noranda-Optioned Borland Lake property in Northwestern Ontario. The program consisted of six diamond drill holes, totalling 3032 feet, designed to test the silver-bearing zones at and below the 300 foot level, and test an area closer to the surface where mineralization had not been established. Drilling by Noranda Explorations prior to 1969 established Probable Ore Reserves of 244,493 tons at 8,27 ounces per ton silver and 0.02 ounces per ton gold. Noranda's exploration delineated the mineral ization to the 250 foot level over a strike length of 1200 feet.As a result of Massive's drill program, the Probable Ore Reserves now stand at 431,967 tons of 8.43 ounces per ton silver and 0.02 ounces per ton gold.

An exploration program consisting of approximately 8000 feet of diamond drilling is recommended to substantially increase the drill indicated tonnage at Borland Lake, and possibly locate other silver-gold deposits either parallel to or along strike of the main deposit. The total cost of the proposed program, if fully implemented, is estimated at $350,000.

PROPERTY LOCATION AND DESCRIPTION

Massive's Borland Lake property is located 125 miles north of the Red Lake gold camp and 50 miles east of the Manitoba border. The property is comprised of a block of 10 leased claims and a contiguous block of 260 unpatented claims for a total of 270 mining claims covering approximately 10,800 acres. Specifically the claims are as follows:

LEASED CLAIMS

Lease No.

102651

102652

BORLAND LAKE AREA

Claim No s.

KRL 49063 KRL 49065 KRL 49066 KRL 50256 KRL 50257

KRL 49059 KRL 49060 KRL 49061 KRL 49062 KRL 49064

Total Leased Claims 10

-5-.

DESCRIPTION OF THE DIAMOND DRILL PROGRAM

A total of 3032 feet of BQ core was drilled in six holes during the period from March 15 to March 29, 1986. The drilling was supervised by the author, and was contracted to M Si B Drilling Ltd. of Powell River, British Columbia, who utilized a Boyles B.B.S. - 15 diamond drill which has a depth capacity of approximately 1000 feet.

The drill equipment was mobilized into Borland Lake via D.C. - 3 and Otter aircraft, and was transported to each drill site by a Bombadier J-5 muskeg tractor. Each drill hole was located and spotted with respect to a chained and picketed grid, with the baseline oriented at 097".

All drill holes were inclined to the north at 45 to 60 0 angle, and were cased through approximately 100 feet of clay overburden using both N.W. and B.W. casing strings. This "double barrelled" casing-string method proved to be extremely effective in stabilizing the hole through to bedrock. Rock-core recovery was excellent, and is estimated to be 9?!!.

GEOLOGY OF THE BORLAND LAKE DEPOSIT

The silver mineralization occurs within two parallel, and roughly east-west striking silicified shear zones. The sheared zones lie in greywacke-type sediments, with the mineralization extending westwards along the structures from an ultramafic intrusive lying stratigraphically to the east. The mineralization consists of varying amounts of sulfide minerals, namely (in order of abundance) pyrite, pyrrhotite, argentite, galena, sphalerite and arsenopyrite. The total sulfide content does not usually exceed 10% with the sulfides occuring as irregular stringers, and disseminations along foliation and shear planes. Hanging-wall alteration occurs as a distinct zone exhibiting up to 10?; garnet porphyroblasts.

Diamond drilling has delineated both the north and south mineralized zones over a strike extent of approximately 1200 feet. The north zone exhibits an average width of approximately 7 feet, with the south zone showing an average width of 10.5 feet. Calculation of the grade-thickness ratio for the south zone suggests that the main body of silver mineralization (Block B) plunges to the southeast at 65 0 (Fig. #3) .

-6-

RESULTS OF THE 1986 DIAMOND DRILL PROGRAM

The purpose of the recent drill program was to test the down-plunge extension of the main zone of silver mineralization at Borland Lake; as well as test an area near to the surface where tonnage had not been delineated. Six drill holes were completed, each hole intersecting both the north and south mineralized shear zones (Fig.#4). The assay results from the six holes are as follows:

Footage ofHole f Section Departure Azmuth Dip Intersection (Ft)MBL 86-1 3+75E 4+25S 004 -50" 330.

409.MBL 86-2 5+25E 4+50S 004 -50 0 318.

MBL 86-3 3475E 5 + 2SS 004 -53" 453.528.

MBL 86-4 2-t25E 3 + 50S 004 -53" 332. 332.426.

MBL 86-5 1+75E 3+25S 004 -53 0 326.368.

MBL 86-6 0+05E 1+75S 004 -45" 176.

0 0

0

00

0 03

58

0

'-340 '-433

'-323

'-459 -533

'-337 '-344'-428

'-343'-376

'-196

.0'

.0'

.2'

. 0'

. 4 '

.4'

.3'

.3'

.0'

.7'

.3'

4 5

Assay

.1602

.51oz

5.3002 over 5

58

14 0.7

1413

19

.2402

.6302

.03oz 044oz.40oz

.50oz

.49oz

.2302over 20

212. 0 '-220 .0' 13 .95o2over 8.

247. 7 '-251 .7' 23 .38o2over 4 .

AgAg

Ag; .2'

Ac)Ag

Ag AuAg

Aq

Ag

Ag ;.3'

over over

10. 24.

0.1 3oz

overover

over overover

overover

6.05.4

5.4 12.2.0

16.7.9

0.0202

0 0

1

1

AU

it

3t

5'

f

'

Au

Ag; 0.055020'A9;

7'0.07o2

Au

Au

Drilling by Noranda Explorations prior to 1969 established Probable Ore Reserves of 244,493 tons at 8.27 ounces per ton silver and 0.02 ounces per ton gold. Noranda's exploration delineated the mineralization to the 250 foot level over a strike length of 1200 feet.

As a result of Massive's drill program, the Probable Ore Reserves now stand at 431,967 tons of 8.43 ounces per ton silver and 0,02 ounces per ton gold (Fig. #5).

Grade Block From To Tons Ag AuA B C

4+25W 2+75W 10,1250+25W 5+75E 383,1856+25E 8+25E 38,657

TOTALS 431,967

8.008.765.23

8.43 0.02

-7-

The greatest potential for additional reserves is at depth under Block B which has been tested to the 400 foot level only. Continuity of this block alone to the 1,000 foot level would effectively double the ore reserves. Other potential areas for additional tonnage are under Blocks A and C and along strike to the east from Block C.

CONCLUSION AND RECOMMENDATIONS

Massive Energy's 1986 drill program increased the Probable Ore Reserves of the Borland Lake deposit by 187,474 tons, to a total of 431,967 tons at 8.43 ounces per ton silver and 0.02 ounces per ton gold. Further drilling is definitely warranted as it has the potential of doubling the present tonnage outlined at Borland Lake .

It is recommended that an 8000 foot diamond drill program be undertaken to further define the silver deposit at Borland Lake. The program would be designed so as to delineate the main block of silver mineralization (Block B) down to a depth of 600 feet, as well as test on induced polarization anomaly as recommended and outlined by Excalibur Consultants Ltd. (J. Boniwell, 1986) . An expenditure of $350,000 is budgeted for this phase of exploration.

PROPOSED EXPLORATION PROGRAM

The proposed exploration program would best be carried out during the winter months, and would consist of the following:

- surveying of grid lines over the ice of Borland Lake and Solon Pond.- complete a V.L.F. electromagnetic survey using the broadcast fields of NLK, Seattle, Washington, and NSS, Annapolis, Maryland to better define E-W and N-S trending structures.

- diamond drill the targets outlined by Excalibur Consultants; 3 drill holes totalling 1250 feet are recommended.- diamond drilling of the main block of silver mineralization at Borland Lake, to delineate the mineralization to the 600 foot level; 7 holes totalling approximately 6750 feet.

The budget for the proposed program is as follows:

- Re-establish grid lines over the ice of Borland Lake and Solon Pond 51,000.00

- V.L.F. electromagnetic survey, two transmitting stations, on all lines, total of 25 line-miles x $90/mile 2,250.00

- Diamond drilling of the main block of silver mineralization at Borland Lake, and test targets outlined by Excalibur Consultants Ltd.; total of 8000 feet x $35/foot, includes mobilization/demobilization, moves, camp and support costs 280,000.00

- Analytical costs; 350 samples x 5 25/sa. 8 ,750.00

- Logging, supervision, report writing and drafting, all inclusive 15,000.00

- Consulting Fees, 10 days x ?4007day

- Fixed Wing Transportation

- Contingencies

4,000.00

20,000.00

19,000.00

Total Exploration Expenditures

September l, 1986 Toronto,Ontario

$350,000.00

n

Kenneth V/. Johnson B. Se, Project Geologist

LIST OF REFERENCE

Boniwell, J. B. 1986

Geophysical Investigations at Borland Lake Area, Red Lake Mining Division Ontario, Massive Energy Ltd. private report.

Bourne, D. A. 1985 Report on Borland Lake Property, Favourable Lake Area, Red Lake Mining Division, Massive Energy Ltd., private report.

Johnson, Ken 1985 Report on Massive Energy's "Borland Outlier" Property, Massive Energy Ltd., private report.

DIAMOND DRILL RECORD BUSH PILOT CORKMATION DC.

Massive Borland Lake498

NAME OF PROPERTY

HOLE NO. MBL 86-1______ LENGTH ^..LOCATION Borland Lake Grid- LATITUDE _____T!________ DEPARTURE

ELEVATION Lake.——————— AZIMUTH 004

4 + 25S

DIP -50"STARTED March 15, 1986 F IM ,^ HFn March 17, 1986

FOOTAGE

398498

DIP

43"430

AZIMUTH

004

004

FOOTAGE DIP AZIMUTH

Of l HOLE NO. O P ~-1 SHEET NO.

REMARKS casing pulled

LOGGED BY .. K. W. JohnsonFOOTAGE

FROM

0

176.0

176.6

181.0

182.7

?01 . 8

^kx

P

TO

176.0

176. 6

181.0

DESCRIPTION

Casing

Granite Boulder

Fine Grained Greywacke- very fine grained, black with moderatefoliation @ 50" to C/A; sporadic garnets exhibited

182.7

201 .8

205.0

in coarse porphyroblasts to 1/8 inch diameter.

Breccia Zone- annealled fault zone; large chloriticclasts in a fine grained micaceous matrix; tracepyrite.

Fine Grained Greywacke-as previous; C/A at 40" with occasionalinterbed of chloritic material.185.6-190.0: becomes more chloritic andbioti tif erous; tight drag folding evident; C/Ashallows to 10", trace pyrite on foliation planes.196.4-196.8: Pegmatite Dyke196.8-201.0: Greywacke; as previous withmoderate foliation at 40 0 to C/A; becomes somewhatbrecciated at 200*.201.0-201.8: Pegmatite.

Brecciated Greywacke-highly foliated at 50" to C/A with chloriticsections.204.0-204.3: quartz-carbonate vein at 30 0 to C/A; drusy quartz with trace euhedral pyrite.

SAMPLE

NO.

86008600

\S Utl PH - IDES

1 Tr2 Tr

FOOTAGEFROM

198. 0203.0

TO TOTAL

203. C208. (

5

5

ASSAYSAu Aa

i; S OZ/TON OZ/TON

i

T rT r

NilNil

DIAMOND DRILL RECORD NAME or pnopEBTY-Massive BorlandMOLE NO.

Lake86-1SHEET NO, .FOOTAGE

FftOM

205.0

218.1

219.2

223.3

224.0

227.7

229. 2

*

TO

218.1

219.2

223. 3

224.0

227.7

229.2

256. 0

DESCRIPTION

Medium Grained Greywacke-massive and biotitiferous with faintbedding foliation at 50 0 to C/A.209. 5~|

211. 8-212. 2jJ Porphyritic dyke; medium grainedwith foliated chloritic selvages, 3% fine grainedpyrite along foliation planes.- at 214.0 large garnet porphyroblastsare evident, up to 1/2 inch diameter.

Pegmatite Dyke- biotite phenocrysts.

Fine Grained Greywacke- weak bedding foliation with occassionalquartz veining up to 2 inches in width, with C/Aat 15"; folding evident at 220.0 feet, shallowangle at 10 0 to C/A.

Pegmatite Dyke

Siliceous Greywacke- moderate to strong foliation at 70" toC/A; up to 204 biotite on foliation planes.

Pegmatite Dyke- slight potassic alteration; very coarsegrained and megacrystic.

Siliceous Greywacke- as previous with moderate foliation at70" to C/A; breccia/debris flow evident at 233 to 236 feet; angular to subangular clasts evident in a siliceous and sericitic matrix. 243.0-256.0: trace to 14 disseminated pyrite; stringers and fracture fillings of pyrite at 60" to C/A.250.0: greywacke becomes garnetiferous

SAMPLE

NO.

8600 860C 8600 860C 9600

^ SUL^M,

IOCS

3 4 U 5 U 6 20 7 Tr

FOOTAOCMOM

238.0 243.0 248.0 t, 2 53. 256.0

TO

243.0 248.0 253.0 0 256 258.0

TOTAL

55 5

0 3 2

ASSAYSAu Aa^ -. O/ NX

T r T r T r Tr Tr

oi ton

Ni 1 Nil Nil Nil Nil

DIAMOND DRILL RECORD NAME OF PROPER-TV Massive Borland LakeHOLE NO. 86-1——————.——————— SHEET NO.______3

FOOTAGE

FROM

256.0

272.5

293.0

302.7

t

TO

272.5

293.0

302. 7

305.4

DESCRIPTION

with 24 disseminated garnet porphyroblasts; mediumgrained.253.6-254.2: sheared and siliceouszone with irregular stringers of massive pyrite.

Fine Grained Greywacke- moderate foliation at 60" to C/A;interbeds evident of more felsic greywacke;occasional porphyroblast of garnet up to 1/4 inchin diameter.

Siliceous Greywacke- moderate foliation with biotitemarking foliation planes in concentrations up to204; siliceous ground mass; foliation at 50" to C/Atrace to 14 pyrite in stringers and along fractureplanes .- pegmatite selvages at 282.0 and292.5.

Fine Grained Greywacke- massive to slightly bedded at 60" toC/A; trace pyrite associated with the siliceousinterbeds .298.0-298.6: broken Ground, faultgoujc.299. 4-299. 8

300.4; Pegmatite Selvage.niotitif erous Greywacke

- moderately siliceous with a strongfoliation, 254 biotite in medium grained aggregatesmarking foliation planes; strong foliation at 60"to C/A; 34 fine grained garnet porphyroblastsevident; 14 fine grained disseminated pyrite withoccasional stringer of pyrite.

SAMPLE

NO.

8600860086018601

MtH.'*, lOtS

8 Tr9 Tr0 Tr1 14

f QOTAGCmow

278.0283.0301 .0303.0

10

283. t288. (303. (306. (

TOTAL

5i 5

23

ASSAYSAu Aa

i 01 TO*

TrTrTrTr

oi row

Nil:NilNilNill

DIAMOND DRILL RECORD NAME OF PROPERTY.

HOLE NO.

Massive Borland LakeSHEET NO.FOOTAGE

FROM

305.4

320.0

344.0

f*

TO

320.0

344.0

356. 1

DESCRIPTION

Fine Grained Greywacke- interbedded sequence of mafic greywackesand siliceous greywackes; bedding at 60" to C/A.-318.3-318.4; Quartz-carbonate vein with massive pyrite mineralization; quartz-carbonateselvages; vein at 50" to C/A.

Siliceous Greywacke- moderate foliation; occasional shearedsection with associated silicification; mineralizedsections throughout; foliation at 60* to C/A;occasional stringers of pyrite proximal to mineral ized zones with stringers at 10" to 70" to C/A.330.5-330.1]331.0-331.6] Mineralized Zone with up to30% pyrite and cerargyrite(AgCl) in quartz gangue; hostgreywacke siliceous and shearc331.8-331.9: pyrite stringers; 40* pyrite.over 1/2 inch widths.332.0-332.5: Pegmatite.333.0-334.6: sheared and chloritized zonewith moderate silicificationand l i d isseminated galena/argentite.335.7-336.0: pegmatite.336.0-337.2: siliceous and seritized zonewith 5% pyrite associatedwith sericitic zones; foliat ion at 50" to C/A.339.2-339.4: quartz vein with 5* pyrite

at selvages; vein at 60 0 toC/A.

Sheared Zone -sheared and chloritized zone with strongbiotite alteration; strong foliation at 50" toC/A; trace pyrite.

SAMPLE

NO.

3601360136013601 8601

860186018601860286028602

d.

86028602

\ IULPN|

IOCS

)

3J5 40 i

7 Tr33 30312

3 Tr4 H

FOOT *GtfftDu

306.0311.3316.0.318.0 319.0

321.0326.0.330.0335.0340.0346.0

351.0356.0

TO

3ii.r316. C318. C319. C 321. C

326. C330. C335. C340. C346. (351. C

356. C363. C

foi*L

5. 34.72.01.0 2.0

5.04.05.05.06.05.0

5.07.0

1

ASSAYSAn Aa

*. Of TON

TrTrTrTrTr

TrTrTrTrTrTr

TrTr

b I TOO

.52NilNil.72Nil

NilNil

4.943.38Nil

I*'HNil

NilNil

DIAMOND DRILL RECORD NAME OF PROPERTY———

HOLE NO. -—————66-1

Massive Borland lakeSHEET N O..FOOTAGE

FROM

356.1

363.0

364.3

371.3

f

TO

363.0

364. 3

371.3

409.6

DESCRIPTION

352.6-353.0: pegmatite353.0-356.1: strongly chloritic andbiotitiferous zone with K pyrite and tracesphalerite in siliceous sections.

Siliceous Greywacke-highly siliceous and altered unit withmoderate foliation at 60" to C/A; strong sericitialteration evident in more siliceous sections.356.6-357.2

358.2: Pegmatite359.0-359.3

362.0: strongly sericitic.

Pegmatite Dyke

Siliceous greywacke-as previous; good interbedded sequenceof alteration mafic and siliceous greywacke.364.8-365.0367.6-368.0: Pegmatite

370.0

Sheared and Siliceous Greywacke- sheared and chloritic greywacke; somesections exhibit up to 31 medium grained garnets;sporadic stringers of pyrite at 60% to C/A;garnetiferous sections carry up to 2% finelydisseminated pyrite.376.4-377. 2377.5-378.0378.6-379.0: Pegmatite; slightly379.3-379.5 potassic382. 2-382.8

381.3-382.0: 2% pyrite in stringers383.6-384.4: chloritic zones; heavyshearing with strong biotite alteration; 2*

SAMPLE

WO.

:

3602J602

8602860286028603

x Juirn, 100

)

)

7j3D

FOOT AGETHOU

365.0368. 0

373.0378.0383.0388.0

TO

368. C373. (

378. C383. (388. C393. (

TOTAL

3.05.0

5.05.05.05.0

ASSAYSAn An

i -. 01 TON

TrTr

TrT rTrTi-

cti ro*

1

Nil jNil j

. 82

.481.00Nil

DIAMOND DRILL RECORD NAME OF

HOLE NO.

Massive Borland LakeR fi- 1 , SHEET NO.FOOTAGE

f ROM

409.6

419.3

' 423.6

f

TO

419.3

423.6

429.0

DESCRIPTION

hornblende?; C/A at 60".386.0-386.2388.3-389.1

390.0: pegmatite; white, slight390.6-391.2 potassic alteration at 389'.392.2393.0

395.5-396.3396.6-398.5: garnetiferous greywacke with404.5-406.0 medium grained porphyro-blasts of garnet; sericitic alteration associated with porphyroblastic texture; trace disseminated pyrite.

Mineralized Shear Zone-highly silicified greywacke, alteredwith average of 51 disseminated and stringerpyrite; cerargyrite evident associatedwith sulfide-rich zones; moderate biotitealteration evident along fracture planes.415.5-416.0: 10% disseminated pyrite andcerargyrite in 'clots' up to 1/4 inch diameter.

Sheared and Chloritic Greywacke-strongly foliated and chloritized zonewith strong biotite alteration; garnet porphyro-blasts evident at 421'; trace to 21 disseminatedpyrite and stringer pyrite; C/A at 50".

Mineralized Zone -3* pyrite/cerargyrite on average in rtisseminations and 'clots'; strong biotitealteration at 45" to C/A.

SAMPLE

NO.

i6031603 5603 J60336033603

8603 3603

t SUL"*f

me*

! Tr 3 Tr 1 5%i 10 !i Tr

7 34 J U

f OOTACEMO"

393.0398.0 403.0 409.0414.0419.0

423.0 428.0

TO

398.0403. C 409. C 414. C419. C423. C

428. ( 433. (

TOTAL

5.05.0 6.0 5.05.04.0

5.0 5.0

ASSAYSAu Aa

i i. 01. TOM

TrTr Tr .01TrTr

0. 04Tr

ot rov

Nil.90Nil

5.06"0.46)1.14

18.3'2.01

check

S.Si*W

18.0

DIAMOND DRILL RECORD NAME OFHOI F MO

Massive Borland Lake86-]

SHEET NO.FOOTAGE

f ROM

429.0

467.0

TO

467.0

471.7

498.0

DESCRIPTION

Siliceous Greywacke

- moderately to slightly sheared withfoliation at 60" to C/A; exhibits sporadic interbedof chloritic material, could be mafic volcanic orultrabasic.

429.2-429.5: 101 garnet porphyroblasts429.9-430.4: chloritic interbed.433.0: foliation becomesdominant at 55 0 to C/A; biotite shards evident.435.8-436.9: chloritic shear zone437.9-439.0: siliceous mineralizedzone with 3% disseminated pyrite.

441.0-441.5445.5

445.7-448.0: Pegmatite450.6-451.3456.3-456,9

460.6: chloritic breccia zone465.3-466.3: pegmatite

Siliceous Greywacke-as previous 483.0-488.0: siliceous sectionwith 21 pyrite; foliation at 60 0 to C/A.

End of Hole

J^ J^~^ w' ifl^^

Kenneth w. Johnson

SAMPLE

"0-

y

3603

8604 86048604

x suim, loci

) 31

0 Tr 1 Tr2 2%

FOOTAGEFflOM

437.0

473.0 478.0482.7

TO

440. C

478. ( 482.'488.1

10HL

3.0

5.0 4. 75.3

ASSAYSAn Aax v Of TON

Tr

Tr TrTr

01 TO*

4.17;

Nil NilNil

DIAMOND DRILL RECORD njst nurr COKKMATKM me.

NAME O F PROPERTY Massive Borland lakeHOLE NO.

LOCATION

LATITUDE

ELEVATIOI

STARTED

MBL ft S-Borl

L5+25Ei I.akpMarch 18,

2and l,

. L ENGTH — ^

ake Grid .

AZIMUTH C

1986 FINiSMEO

|Qft feet

4+50S*n4 oMarch 20,

DIP -^n 01986

FOOTAGE

300'498'

DIP

-4 2 o-37 0

AZIMUTH

004

004

FOOTAGE DIP AZIMUTHMBL

REMARKS Casing pulled

LOGGED BY Kenneth W. JohnsonFOOTAGE

FROM

0

137.0

138.6

149.5

11

TO

137.0

138.6

149.5

174.4

DESCRIPTION

Casing in Overburden

Broken Core; Boulder Material

Interbedded Greywacke Sequence

- fine to medium grained greywackesinterbedded with sericitic greywackes; moderatefoliation at 70 s to C/A; some of the more siliceoussections are highly garnetiferous.

Mineralized Garnetiferous Greywacke- moderately to strongly sheared and silicified with strong foliation at 50 0 to 60 0 to C/A; garnets are porphyroblastic and medium grained; trace to 11 pyrite in disseminations and stringers; stronger porphyroblastic texture indicative of strongest mineralized sections.

149.5-150.0: 2% pyrite in slightlygarnetiferous and siliceous greywacke; moderateshearing .

150.0-152.0: sheared and garnet iferous greywacke, moderate biotite alteration;trace disseminated pyrite; shearing at 60" to C/A.152.U-152.4: annealled f&ult gougewith 3* disseminated pyrite.152.4-153.2: garnetiferous grey wacke with H pyrite.153.2-154.6: fault gouge, partially

SAMPLE

NO.

860486048604 8604 8604 8604 8604 8605 8605

^1"

3 U4 5%5 4* 6 Tr 7 34 8 3 1 9 Tr 0 Tr 1 Tr

FOOTAGEFROM TO

1

149.0153.0158.0 163.0 166.0 168.0 173.0 178.0 183.0

TOTAL

153.0 4.0158.0163.0 166. C 168. C 173. C 178. C 183. C 188. C

5.0

5.0 3.0 2.0 5.0 5. 0 5. 0 5.0

ASSAYSAu Aa

^ S OZ/TON

TrTrTr Tr T r T r T r Tr T r

OZ/TON

NilNilNil Nil Nil Nil Nil Nil Nil

DIAMOND DRILL RECORD NAME OF PROPERTY. Massive ^Borland LakeHOLE NO. MBL 86-2

SHEET NO..FOOTAGE

FROM

174.4

178.2

"

TO

178.2

185.0

DESCRIPTION

annealled with thin quartz-carbonate stringers evidentin broken core, 5% to 1 01 pyrite at stringer selvages;at 154.1 large pyrite clast, rounded, are evident andare composed of 6(H pyrite.

154.6-158.5: garnetiferous greywackewith up to 2% disseminated pyrite.158.5-158.9: 4% pyrite in stringerswithin garnetiferous greywacke.158.9-166.0: garnetiferous greywackewith pegmatite selvages at 163 feet.166,0-171.8: Mineralized GarnetiferousGreywacke: 10% garnet porphyroblasts with up to 3% disseminated pyrite; strong foliation at 60" to C/A;strong biotite alteration.166.7-167.1: fault gouge with up to 401massive pyrite.171.8-173.3: potassic pegmatite dyke.173.3-174.4: 101 garnet porphyroblasts.

Potassic Pegmatite Dyke

-highly siliceous and megacrystic withtrace pyr i Le.

Mineralized Shear Zone

-heavy shearing and silicificationevident with pyrite mineralization up to 10?. over shortsections; shearing at 50" to C/A.180.2-181.7: quartz-rich section withup to 10* fine grained pyrite in irregular stringers,shearing at 50 0 to C/A.183.5-185.0: silicified and shearedgreywacke with 5% disseminated fine grained pyrite.

SAMPLE

NO.

!6051605 !605J605i6055605)605

* SULPM,

lOCi

3

t

t1

l

FOOTACtmow

188.0190.5 195.6198.2203.4208.4209.4

TO

190. 5(195.6 198.2]203.41208.4209.4218.0

rtmi

2.55. 1 2.65.25.01.08.6

ASSAYSAn An

\ 1 02 TOW

TrTr TrTrTrTrTr

01 TOW

NilNil NilNilNilNilNil

DIAMOND DRILL RECORD NAME OF

HOLE NO. MBL 66-2Massive Borland Lake

SHEET NO..FOOTAGE

FROM

185.0

195.8

198.0

i

205.6

206. 7

1208.0

TO

195.8

198.0

205.6

206.7

208.0

218.0

DESCRIPTION

Sheared and Siliceous Greywacke- moderately sheared and siliceous grey wacke with strong to moderate foliation at 50" to C /h;becomes garnetiferous at 191.0'192.0-194.0: garnetiferous section(10* .garnet porphyroblasts) with 11 stringer pyrite;sulfide-filled {pyrite) fault gouge at 192.8; vuggywith pyrite crystals.194.0-195.6: quartz vein with contactsat 50" to C/A; biotitiferous selvages.

Mineralized Garnetiferous Greywacke- 20% garnet porphyroblasts in abiotitiferous matrix; strong foliation at 70 0 to C/A;fine grained stringer pyrite in concentrations of 51on average.196.8-197.8: massive quartz-pyri tccarbonate vein; *W pyrite on average.

Interbedded Greywacke Sequence- interbedded sequence of fine grainedintermediate to felsic greywacke; good bedding at 60"to C/A.203.0-205.0: garnetiferous greywackesilicious with trace disseminated pyrite.

204.5: fractures at 10" to C/Awith trace pyrite.

Garnetiferous Greywacke Sequence- as previous; trace pyrite.

Interbedded Greywacke Sequence- interbedded greywacke sequence withbedding at 70" to C/A.

Garnetiferous Greywacke- garnet porphyroblasts dominate withhighly siliceous sections exhibiting trace to 1* pyrite

SAMPLE

*o. *SUl*Hr

ionFOOTAGE

moM TO TOTAL

ASSAYS

v 1 of row 01 TOM

1

DIAMOND DRILL RECORD NAME OF PROPERTY..—

MOLE NO. MBL 86-2Massive Borland Lake

SHEET NO. .FOOTAGE

rpOM

218.0

260. 3

270. 5

l 308.0

l

TO

260.3

270.5

308.0

319.5

DESCRIPTION

in irregular stringers.208.0-208.3: massive pyrite associatedwith quartz-carbonate stringer; same radiating crystalsof Marcasite; vuggy texture exhibits good cubic crystalssilver in colour.

Fine Grained Greywacke- fine grained greywacke with a moderatefoliation marked by biotite shards, becomes progressive]richer in biotite down-hole; foliation at 60" to C/A;some interbeds of felsic greywacke evident.221.2-222.3: fault gouge with quartz-carbonate stringers and massive pyrite mineralization;some foreign granitic material.226.7-227.7: pegmatite.

230.0: greywacke becomes rich inbiotite; strong foliation at 35" to C/A.236.0-236.5239.5-240.3: pegmatite dyke.248.5-249.0249.7-251.2

Pegmatite - some greywacke material interspersed

Greywacke- as previous with moderate to slightfoliation at 50" to C/A.273.4-274.2: pegmatite276.3-277.3: breccia zone with pyriteinfillings; up to 15* pyrite total.278.4-281.6: pegmatite breccia zone;2% pyrite along fractures at 281.0.302.8-303.2: pegmatite.

Garnetiferous Greywacke - heavily sheared section of greywackewith 5% garnet porphyroblasts , strong foliation at 60"

SAMPLE

NO.

1

y3605

8COC

8606 860(860C

* mi*-,IDtS

9

0

1 23

FOOTAGEnou

220.3

276.0

308.0 313.0318.0

TO

222.4

278.

313. 318.323.

TOTAL

2.1

i 2.0

1 5.0 ) 5.0i 5.2

ASSAYSAu Aa

i \ 01 TD*

Tr

T r

0. 01 0.010.13

(It 10-

Nil

Ni 1

Nil Nil

5. 3 0

DIAMOND DRILL RECORD NAME OFHOLE NO. MBL 86-2 .

Massive Borland LakeSHEET NO.FOOTAGE

rftOM

319.5

323. 3

1

TO

323.3

362.8

DESCRIPTION

to C /A: up to 5% pyrite in more garnet-rich sections,overall 2% pyrite; dragfolding evident at 318.0.313.0: quartz-carbonate vein with 21pyrite.

Fine Grained Greywacke- as previous; slightly garnetiferouswith slight foliation and/or bedding at 50' to C/A.

Garnetiferous Greywacke- slightly garnetiferous at 323.3 andbecomes progressively more so down hole; trace to l istringer pyrite associated with the garnet zones.326.0-326.2: stringer of pyrite-galona-argentitc in concentrations of 5%.327.2-328.0: pegmatite.328. 0-328. 5: quartz-carbonate-pyritevein with trace argentite.

329.5: galena-argentite stringer;1/4 inch in width.330.6331.5: quartz-carbonate-pyrite332.5 stringers at 50" to C/A.333.4

331.5332.6: quartz-carbonate-pyrite337.6 stringers at 50" to C/A.338.6

336.6-336.9: potassic pegmatite.340.8-341.6

329.0-330.0: 2% stringer pyrite insheared greywacke; quartz-biotite-garnet matrix; strongfoliation at 50 0 to C/A.

SAMPLE

NO.

860i860i8601860i860'

860860

IOCS

45678

90

FOOTAGEFftOu

323.2328.4332.9338.2343.3

348.7352.0

TO

328.4332.9338.2343.3348.7

352.0357.0

TOTAL

5.24.55.34.15.4

4. 75.0

ASSAYSAn Aai or rot

TTTrTrTrTr

TrTr

01 TON

NilNilNilNilNil

NilNil

j

DIAMOND DRILL RECORD NAME OF PROPERTY.

HOLE NO. M B L 86-2

Massive Borland LakeSHEET NO..FOOTAGE

r ROM

362.8

378. 3

U17.8

f

TO

378.3

417.8

429.2

DESCRIPTION

341.6-357.0: 4% disseminated pyrite,trace argentite in highly siliceous and garnetiferousgreywacke; strong foliation at 40" to C/A; good sulfidestringers associated with quartz-carbonate stringers.357.0: fault gouge; broken core.357.6-362.8: heavy shearing; strongbiotite alteration; shear selvage.

Siliceous Greywacke- medium grained siliceous greywackewith occasional interbed of mafic greywacke; foliationat 55" to C/A.

376.3: quartz-carbonate-pyritestringer at 55" to C/A.

Biotitiferous Greywacke- garnetiferous at top of section becomirprogressively more micacious down hole; at 381.0 becomesvery schistose with strong schistosity at 60" to C/A;trace disseminated pyrite along foliation planes.387.0-388.2: sheared and chloritizedsection; could be mafic intrusive.388.2-389.0: siliceous section.389.0-390.6: fault gouge.391.6-393.9: sericitic greywacke.moderately sheared and siliceous with clots of sericiticmica; very fine grained.399.4-401.2: potassic pegmatite dyke.404. 7-405.1

411.3-417.8: sheared and siliceous zonewith up Lo 2* pyrite in disseminations and irregularstringers; moderate foliation at 60 0 to C/A.

Sheared Mafic Intrusive- highly sheared and chloritized andbioti tif erous sections with 2% stringer and ^isseminatec

SAMPLE

NO.

J

86078607860786078607

X iUl'K,

IOC1

1234 2 1,3

FOOTAGEr.ou

407.0412.3417.0420. 0429. 3

TO

412.:417. (420. (429. .434.

TOTAL

3.34. 73.09. 35.0

ASSAYSAn An

\ 01 TOW

TrT rT rT rT r

01 TOD

1

i

i

NiltillNilNilNil

DIAMOND DRILL RECORD NAME OF Massive Borland LakeHOL E NO MBL 86-2 SHEET NO.FOOTAGE

FROM

129.2

K

TO

98.0

498.0

DESCRIPTION

pyrite; weak foliation at 70" to C/A; appears massive,slightly carbonated; probably sheared peridotite,slightly talcose.429.0: galena-argentite stringer,1 inch in width.

Siliceous Greywacke- massive and fine grained siliceousgreywacke; exhibits fine grained shards of biotite at2%; trace pyrite in occasional stringers.432.6-432.9: pegmatite.447.1-448.1: breccia zone; broken core- at 450.0 thin fractures filled withquartz are evident; dominantly at 50 0 to C/A.

End of Hole

Kenneth W. 'johnson

SAMPLE

MO. * SUl'M,

IOCSFOOT AGt

MOM TO TOTIl

ASSAYS

v1 Of TON 01 fOM

!

l/)t

MJSH MLOT COftrOftATION INC.DIAMOND DRILL RECORDNAME OF PROPERTY Massive Borland Lakeun . r ^ M BL 8 6 ~ 3 ,E N r.TM fidfi Feet, NATION Borland Lake Grid . . .ELEVATION Lake AZIMUTH 004" DIP -5.1"

M^.v-^.1-, -51 IQRf, Mjar-^h 7/1 1QRK

FOOTAGE

426600700

ppv

DIP

-43 0-38 0-34 0

AZIMUTH

004

FOOTAGE DIP AZIMUTHj Rfi-

REMARKS - . Csiai n g Pill 1 ort

LOCOED BY ,Kenneth W. Johnr-.qnFOOTAGE

FROM

0

236.0

238.2

238.8

240.4

252. 4

276.0

280. 8

T*

TO

236.0

238.2

238.8

240.4

252.4

276.0

280.8

294.0

DESCRIPTION

Casing in Overburden

Boulders; granitic and sedimentary in origin.Greywacke

Potassic Pegmatite Dyke

Siliceous Greywacke - highly siliceous greywacke with moderate foliation at 70" to C/A; medium grained with clasticappearance. 250.5-252.4; potassic pegmatite dyke.

Sheared Zone- highly schistose and micaceous zone; primary textures not readily observable; strong schistosity at 60"; some sections pegmatite; all sections very soft and friable (fault zone?).

Siliceous Greywacke - as previous; becomes sheared at 278.0.

Mafic Intrusive- sheared and foliated mafic intrusivegabbro, or mafic volcanic; exhibits some intercalate greywacke sections; shearing evident at 60 0 to C/A; chloritic and biotitif erous.

SAMPLE

NO.

1

WTFOOTAGE

FROM TO TOTAL

ASSAYS

V x 02/TON OZ/TON

DIAMOND DRILL RECORD NAME OF PROPERTY. Massive Borland LakeMBL 86-3

SHEET NO. .FOOTAGE

f ROM

294.0

299.1

322.8

344. 3

T

to

299.1

322.8

344.3

356.0

DESCRIPTION

Siliceous Greywacke- as previous

Sheared Mafic Intrusive- appears gabbroic; moderately sheared tomassive in some sections.309.8-315.6: becomes porphyritic with 2%feldspar porphyroblasts.320.0-322.8: white pegmatite.

Greywacke- moderately foliated and siliceous,foliation at 70" to C /h; some interspersed gabbroicsections, foliated and sheared greywacke bounds thegabbro.325.0-326.0: quartz vein, bull white at60" to C/A.- becomes sheared and moderatelybiotitifcrous at 336.0 feet; foliation at 70 0 to C/A.338.2: quartz-carbonate stringer at342.6 50 0 to C/A, with pyrite at

selvages.

Mineralized Greywacke- sheared and siliceous greywacke withmoderate foliation at 70 0 to C/A; up to 3% stringerpyrite associated with the more siliceous sections;strongly bioti tif erous with gneissic-like bands ofalternating siliceous and biotite-rich sections.347.2-349.3: game tif erous-siliceousgreywacke; porphyroblasts of garnet up to 1/4 inchin diameter oriented along foliation planes inconcentrations up to 54; l i d isseminated pyriteassociated.349.5-352.7: 34 pyrite in stringers at 10to 60" to C/A; associated with siliceous zones;trace AgCl.

SAMPLE

NO.

8607860786078607860886088608

X SUL'H,

toes

6789012

FOOTAGEmow

336.0341.0346.0351.2356.0361 .0366.5

ID

341.!346. (351.:356.1361.1366.!371.!

101*1

5.05.05.24. 85. 05. 55.0

7^5AVS Agi \ 01 TON

T rTrT rTrT rT rTr

(it TON

NilNilNilNilNilNilMi 1

DIAMOND DRILL RECORD NAME OFHOI F MO MBL 86-3

Massive Borland LakeSHEET NO.

FOOTAGE

FROM

356.0

358.0

364.5

369.4

ItT

TO

358.0

364.5

369.4

444.3

DESCRIPTION

354.0-356.0: pyrite in irregu lar stringeBrecciated Greywacke

- siliceous fragments in a medium grainedmassive matrix.

Siliceous Greywacke- as previous; slight foliation at 70" toC/A.

Mineralized Greywacke- as previous with 21 pyrite stringerswith biotite-rich sections.

366.5: trace AgCl

Siliceous Greywacke- moderately foliated at 60" to C/A; biotishards mark foliation planes.

374.6376.6: trace pyrite associated with384.4 siliceous zones.387.2

390.6-392.0: sheared and siliceous zone;strong foliation at 50 C to C/A; quartz vein at391.5-392.0; trace pyrite.392.0-393.8: slightly garnetiferoussection; in biotite-rich and siliceous zone; 2*stringer pyrite associated with siliceous zones.402.5

403.7: fault gojge.404.9

407.0-408. B412.0: sericitic alteration with412.6 porphyritic-serici tic in413.4-413.8 disseminations.

SAMPLE

NO.

S

i608i608!6085608S608)608 J6083609

:O

\ SUL**( lOt)

3i

i

)1

3 3)

FOOTAcernoM

386.5391.5396.5401.5406.5411.4 416.5421.4

ro

391.5396.5401.5406.5411.4416.5 421.4425.9

TOTAL

5.05.05.05.04. 95. 1 4.94.5

A KV YS Ag-. \ 01 TON

TrTrTrTrTrTr TrTr

ffi T OM

NilNilNilNilNil \Nil NilNil

DIAMOND DRILL RECORD NAME OF PROPERTY- Massive Borland LakeHOLE NO. MBL 86-3

SHEET NO..FOOTAGE

FROM

444.3

451.0

468.5

487. 8

It• 01.1

TO

451.0

468.5

487.8

501.1

504.9

DESCRIPTION

418.8-421.0: siliceous zone with slightbiotite alteraion, up to 3% disseminated pyriteassociated with siliceous sections.442.3-444.3: 2% pyrite in stringers assoc iated with siliceous sections.

White Pegmatite- fine to medium grained dyke; very siliceousno mineralization noted.

Mineralized Greywacke - siliceous section with moderate shearingevident; trace biotite alteration; 5% stringerpyrite evident in siliceous sections trace to J.%Marcaskic pyrite.458.0-459.0: 5% pyrite in siliceous andsheared section; H galona-argentite evident.

Siliceous Greywacke- very fine grained and siliceous with slightfoliation at 70 0 to C/A.468. 5-471 . 0471.4-472.6: shear zone; chloritic and473.5-474.0 siliceous

478.0-478.5: ground core.480.8-481.0: white pegmatite.

Pegmatite Dyke- sheared and slightly potassic.491.2-492.8: greywacke

498.0: ground core.498.0-499.5: sheared and potassic zone withtrace to H pyrite on fractures.

Sheared Zone- highly chloritic and bioti bif crous with

*4O.

!609

8609 860986098609

t StHPH, IOCS

.

2 313

SAMPLE

F~OOT~AGSF*OM

441.2

453.0 456.0459.0464.0

10

446. 0

456. C 459. (464. (468. i

rOTAL

4. 8

3.0 3. 05.04. 8

i

ASSAYS————— . ______ a 11 ftfi ____ _

i or 'ON

Tr

Tr 0.02TrTr

—— —3 ———

01 row

Nil

Nil 9.84NilNil

DIAMOND DRILL RECORD NAME OF pROPERTv—^Jlaaal^ii.^Borlan.d Lake HDI F no M BI. B6-3 sneer NO.FOOTAGE

FfiOM

504.9

518.0

533.1

IO

518.0

533.1

579.5

DESCRIPTION

strong foliation at 35" to C/A.

Siliceous Shear Zone- sheared and silicified zone with bandingof silica-rich sections; biotite shards mark slightfoliation at 70 0 to C/A; trace pyrite noted.510.4; stringer of Marcasiticpyrite at 70" to C/A.

514.0: trace argentite along fract ure plane.

Garnetiferous Greywacke- siliceous and sheared greywacke withgarnetiferous sections throughout; porphyroblastictexture, slight to moderate foliation at 70" to C/A.531.5-533.1: potassic pegmatite,sericitic alteration along fractures.

Mineralized Greywacke- siliceous and sheared section with up tcS 1* pyrite in stringers and disseminations; moderatebiotite alteration associated with sheared sections.trace Lo 3% argentite-galena over short, shearedsections; foliation at 65 0 to C/A.535.1-537.0: stringer and disseminatedargentite-galena; in concentrations to 3%.539.0-540.0: 3% pyrite stringers ingarnetiferous greywacke.548.9-549.9: 10*. pyrite stringers ingarnetiferous greywacke; 31 Cerargyrite (AgCl)associated with sulfide-rich sections.

550.7: trace argentite.562.0-563.5: 10i irregular pyritestringers with 5% cerargyrite associated.566.7: quartz-carbonate stringerwith l Ot, pyrite.

SAMPLE

NO.

!60956095609560956108610861086108610

8610861C861C861C861086118611

tlUl'H,

IOCS

)

7

i

)

)

1

234

5678901

FOOT AGEmoM

504.5508.0513.0528.0533.4535.0538.0543.0548.0

553.0558.0563.2568.0573.0577.0582.0

TO

508. 0513.0518.0533.4535.0538. (543. (548. (553. (

roT*t

3.55.05.05.41.63.05.05.0

i 5.0

558.6 5.0563. i 5.2568.6 4.8573.? 5.0577. (j) 4.0582.587.

l 5.0l 5.0

ASSAVSAll An

•; 01 TO*

TrTrTr

0.03TrTrTr0.030.05

0.03TrTrTr

0.04Tr

0. 02

6i 10*

NilNilNil

8. 63Nil1.13Nil

1.71Nil

5.004

2.82Nil,NilNil:

2. 93|Nil]Nil

o'

DIAMOND DRILL RECORD NAME or PROPERTY Massive Borland Lake KOI F MO MRT. 86-3_______ SHEET NO,_

FOOTAGE

f ROM

579.5

650 .4

656.3

684 .7

692.7

r

TO

650.4

656.3

684.7

692. 7

698.0

698.0

DESCRIPTION

566.8-572.0: sheared and chloritic section;moderate to strong foliation at 70 0 to C /h.572.0-576.7: siliceous mineralized greywackeweak foliation development exhibited; trace to 11biotite shards; trace to 11 stringer and disseminatedargentite associated with siliceous sections. 574.4-575.2; 2% argentite along fractureplanes.576.1-579.5: sheared and chloritic greywackemoderate to strong foliation at 40" to C /h; biotite-rich partings mark foliation planes.

Siliceous Greywacke- moderately sheared and silicified greywackeslight foliation at 50" to C /h; trace pyrite on fracturplanes.579.9-580.6: siliceous zone.595.6-596.4

599.6-600.4: quartz veins at 50".631.0: fractures at 50 0 .

White Pegmatite

Fine Grained Greywacke- foliation at 65" to C/h.

White Pegmatite- interf ingered greywacke evident.

Siliceous Greywacke- foliation at 65 0 to C /h.

End of Hole.

Kenneth W. Johnson

MO.

!

a SULPX,SAMPLE

FOOTAOC

ASSAYS

-, •V 01 TO* fit TDK

1

DIAMOND DRILL RECORDNAME OF PROPEHTV Massive Borland Lake——————MSL 86-4 .,^,. u 498 Feet

KISH mor couoiuTtON INC.

HOLE NO.

LOCATION ROT" LATITUDE L2+25E ELEVATION Lake

LENGTH

e GridDEPARTURE

. AZIMUTH

3 + 50S

STARTED,March 24, 1986 FINISHED,March 26. 1986

FOOTAGE

363'498'

DIP

450

42"

AZIMUTH

004

FOOTAGE DIP AZIMUTHHOLE NO. fifi-4 SHEET NO. .

Casing pulledREMARKS.

LOGGED BY Kenneth W. JohnsorxFOOTAGE

FROM

0

159.0

195.9

f

TO

159.0

195.9

210.5

DESCRIPTION

Casing in Overburden

Greywacke- moderate foliation at 50" to C/A;moderately biotitif erous and medium grained.

169.6: quatrz vein with sericitealteration along selvages; strong schistosity at45 0 to C/A.169,7-171.4; quartz-carbonate vein at40" to C/A; exhibits silicified selvages; nomineralization noted.172.6-174.3: sheared and silicified176.0-177.0: section with epidote?alteration; trace pyrite sporadic garnets.

179.8180.8-182.2

183.0: sheared and garnetiferous185.4 zone with moderate foliatio;188.0-188.7 at 40" to C/A.189.0

- at 191.0 greywacke becomes siliceous;strong shearing evident at 193.0.

Mafic Intrusive- moderately to highly shearedSerpentinized Peridotite; talc-silicate alterationalong fracture planes; highly biotite-rich withbiotite porphyroblasts marking foliation planesat 50" to C/A; moderately to highly chloritic;hematite noted along fractures at 90" to C/A.

SAMPLE

NO. SULPH IDES

FOOTAGEFROM TO TOTAL

ASSAYS

X ? OZ/TON OZ/TON

i

DIAMOND DRILL RECORD NAME OF PROPERTY.

nr*i f urt O D—M

Massive Borland Lake

SHEET NO. .FOOTAGE

FROM

210.5

227.9

234.8

241. 6

"

J248.2

TO

227.9

234.8

241.6

248.2

281.8

DESCRIPTION

Greywacke- fine grained biotite shards markfoliation planes at 60" to C/A.

210.5-211.1: sheared greywacke withtrace pyrite along shear planes.212.0-212.9: sheared and chloriticzone.212.9-227.9: biotitif erous greywacke,strongly biotite-rich with strong foliation at 60" toC/A.215.0-215.2216.3-216.7: White Pegmatite217.0-217.5218.0-218.3

Siliceous Greywacke- fine grained with trace pyrite alongfracture planes; moderate biotite phenocrysts markfoliation at 60 0 to C/A.231.0-231.2: garnet phenocrysts evident- pyrite stringer with carbonateselvages evident at 230.9 feet.230.9-234.8: trace pyrite alongfoliation planes.

Sheared Greywacke- moderate shearing a t 5 0" to C/A; biotashards mark foliation planes.

Biotitif erous Greywacke- strongly biotitif crous in sectionswith siliceous zones throughout; trace stringer pyrite;strong foliation at SO 0 to C/A,245.3-246.0: Potassic Pegmatite Dyke.

Siliceous Greywacke- moderately to highly siliceous grey-

SAMPLE

NO.

86118611861186118611

to

\ 1ULPM, IDf)

234)

6

FOOTA06FROM

228.0232.7238.0243.0248.0

TO

232.'238. (243.1248. (253. (

TOT*L

4.75.35.05.05.0

tfu* 1' 5 Ag-. -. 01. TON

TrTrTrTrTr

01 TOM

1

NilNilNilNilNil

DIAMOND DRILL RECORD NAME OF PROPERTY. Massive Borland LakeHOLE NO. MSL 86-4

SHEET no..FOOTAGE

FROM

281.8

288.2

|1329.5

TO

288. 2

329.5

331.8

DESCRIPTION

wacke with slight foliation evident , marked bydisseminated biotite shards; foliation at SO 0 toC/A.253.6-253.9: White Pegmatite.259.9-260.5: 44 stringer pyrite insheared biotitif erous zone.260.5-261.9: Potassic Pegmatite.262.5-263.5: siliceous breccia zone.267.0: 2% stringer pyrite at 40 0to C/A in sheared and biotite-rich section.267.7-268.0: White Pegmatite268.5-268.9

273.5: quartz-carbonate stringerat 40" to C/A with 54 euhedral pyrite crystals.274.4-281.8: sheared and garnetiferousgreywacke with 14 stringer pyrite associated withbiotite-rich sections; moderate to strong foliationat 50 0 to C/A; sporadic garnets evident, porphyro blastic up to 1/4 inch in diameter.

Interbedded Greywacke Sequence- interbedded mafic and chloritic grey wacke sequence; remnant bedding at 50 0 to C/A.Siliceous and Sheared Greywacke

- some garnetiferous sections; quartzveining at 40" to C/A at 292.0 feet.- becomes massive and very siliceous at300 feet.322.7-323.5: Pegmatite selvage.

327.2: Pegmatite.328,0-328.3328.4-328.9: biotitif erous and sheared;strong foliation at 60 0 to C/A.

Potassic Pegmatite Dyke- megacrystic

SAMPLE

MO.

5611

)611

t SULPN,

IOCS

t

f DOT ACEfftOM

258.0

273.0

TO

260.0

279.1

TOIAl

2.6

6.1

A!SQVS Aq-.

: h

-. 01. TOM

T r

Tr

01 TON

Nil

Nil

DIAMOND DRILL RECORD NAME OF PROPER-TV Massive Borland Lake HOLE NO. MSL 86-4————— SHEET NO. .

FOOTAGE

FROM

331.8

344. 0

347.0

356.0

378.9

|1

TO

344.0

347.0

356,0

378.9

426.2

DESCRIPTION

Mineralized Greywacke- highly sheared and siliceous zonewith up to 5ri stringer pyrite and 31 galena-argentite in irregular disseminations, foliationand shearing at 55" to C/A; some chloritic shearzones within section carry trace of AgS.331.6-333.4: 5% pyrite in thinstringers at 55" to C/A.334.5-336.7: chloritic zone with 3*istringer pyrite and trace, argentite; somewhatbrecciated.337.6-343.0: up to 3% galena-argentite associated with pyrite-rich and siliceoussections.

Brecciated Greywacke.

Siliceous Greywacke- siliceous greywacke which becomesgarnetiferous at 355.0 feet.

Garnetiferous Greywacke- highly garnetiferous in sections;matrix of siliceous greywacke; trace pyrite inmatrix .361.6-363.2: 21 pyrite in stringersalong foliation planes, in sheared and silicifiedsections; foliation at 50" to C/A.364.0-364.8: 10% stringer pyritein irregular clots and along foliation planes.367.0-369.1: White Pegmatite.

Greywacke- medium grained and foliated at 60"to C/A; slightly garnetiferous in sections; tracedisseminated and stringer pyrite.386.6-387.0: Pegmatite

387.5

SAMPLE

NO.

86118612861286128612

8612861286128612

t SULFX,

1015

}

DJ23

4567

POOTACErftOM

327.0332.0337.4341.6344.3

359. 7365.0369.9373. 2

TO

332. C337.'341. f344.348. C

305.369.373.379.

TOTAL

5.05.44.22.73.7

5. 34.9

23.3) 5 . 8

ASSAYSAu Aa-. or TON

Tr0.040.060.03Tr

T rTrT rT r

01 TON

Nil14.0NilNilNil

|

NilNil

1 . 500. 90

DIAMOND DRILL RECORD NAME OF PROPERTY. MH, r.o MSL 86-4

Massive Borland LakeSHEET NO..

FOOTAGE

F HDM

426.2

437 .4

462.5

|n1

TO

437.4

462.5

498.0

498.0

DESCRIPTION

390.0-390.8: massive pyrite (40%)with quartz gangue; sheared selvages at 60" to C/A.396.0: clay seam.

404.0-405.7: White Pegmatite.413.1-414.2: brecciated greywackewith trace pyrite.421.3: pegmatite.

Mineralized Greywacke- sheared and silicified zone with upto 10% galena-argentite over short sections (6 inchesaverage) ; l i d isseminated pyrite associated with thesiliceous sections.427.0-427.8: 1 QI galena-argentite inirregular stringers, 5% pyrite stringers associated.

Greywacke- slightly sheared and chloritizedsections exhibit good foliation at 60" to C/A;most sections medium grained and massive.442.0-442.4: quartz veins withbiotitc-rich selvages at 50 0 to C/A.444.5-445.0: White Pegmatite.446.3-447.1

458.0-458.9: brecciated greywacke461.0-462.5

Siliceous Greywacke- massive to bedded greywacke withbedding and slight foliation at 50" to C/A.489.2-489.6: White Pegmatite.

End of Hole.

/(U L ' V—Kenneth W'. JohnsonMarch 27, 1986

SAMPLE

NO.

5612

8612861386138613

t SIH'N, rOC!

3 401

3D 10!1p

FOOTAGEMOM

389.:

424.0426.

428.3431.0

10

392.

426.21 428.431. C434. C

TOTAL

0 2.9

2.33 2.0

2. 73.0

AWS Ag^

F

\ 01- TOM

Tr

T r0.01TrT r

t,l I0i

Nil

Nil7. 40Nil

0. 84

DIAMOND DRILL RECORD ipc- KISH fUOT COXKXtATlON INC.

NAME OF PROPERTY

HOLE NO. MBL P6-

LOC A T ION

LATITUDE

ELEVATION

Massive Energy Limited500 feet

Borland Lake Grid1 + 75E

DEPARTURE

.AZIMUTH ^.

3+24SQQ4

26, 1986 March 28, 1986-53

FOOTAGE

dollar300

500

DIP

-53-48

-46

AZIMUTH

004

FOOTAGE DIP AZIMUTH

REMARKS.

LOGGED OY Peter EitutisFOOTAGE

F ROM

0

141.2

159. 3

1

TO

141.2

159.3

DESCRIPTION

Casing In Clay Overburden

Greywacke- moderately foliated with foliation

rich in biotite shards.- foliation at 40" to C/A.

184.5

148.0-148.2: Pegmatite - slightly155.0-155.5 potassic.

158.0: Ground core158.9: small fractures with

talc S carbonatealteration.

Siliceous Fine Grained Greywacke- slight foliation at 40" to C/A- foliation has trace PYRITE166.5-168.0: sheared pegmatite

with slight greenishquartz .

172.7-173.3: sheared greywacke withslight garnets.some chloritic alterataround garnets.stringers at quartz-carbonate with tracepyrite.

175.0-175.6: q tz-carbonate vein at15 0 to C/A.

SAMPLE

NO.

on

*SULPH IDES

FOOTAGEFROM TO

i

TOTAL

ASSAYS

* * OZ/TON OZ/TON

DIAMOND DRILL RECORD NAME OF Massive Energy Limitednni F NO MSL 86-5 SHEET NO.

FOOTAGE

r ROM

184.5

187.2

j

1

TO

187.2

209.0

DESCRIPTION

176.0-176.4: garnets in greywacke-176.4-178.2 slight fractures at15 0 to C/A.

-filled with chloriticcarbonate alteration

-qtz S pyrite crystalswell developed.

178.2-179.8; greywacke withincreased biotitealong foliation.

179.2-181.1: SHEARED PEGMATITE181.1-184.5: zones of garnets andchlorite- carbonatestringers in siliceoigreywacke.

Siliceous Sheared Greywacke- has quartz phenocrysts and somechloritic alteration.- small stringers rich in talc at20" to C/A

187.2: lost core

Mafic Intrusion- highly to moderately shearedperidotite- talc-silicate along fractureplanes- some carbonate alteration also- biotite porphyroblas ts alongfoliation at 40" to C/A.187.2-189.8: chloritic alteration206.0-209.0 along contact of

mafic intrusion.

209.0-211.0: PEGMATITE

SAMPLE

MO.

t

S

x iuon tIOCS

FOOTACfrnoM TO TOT*l.

j

ASSAYS

\ Ot- TON til TON

j

l

l

DIAMOND DRILL RECORD N AM E OF PROP t K i v- ... .Ma s s i y c Energy Limited HOUe NO MBL 86-5 iMtf-T NO.,TOO

rwOM

209.0

229. 3

r AGE

TO

229.3

258.0

OESCWTION

Greywacke - fine grained biotite shards alongfoliation planes at 40" to C/h- trace pyrite along foliation- chlorite alteration spotty and parall(to foliation218.0-218.6: broken core

- carbonate alteration alonefractures parallel tofoliation

220.3-226.0: increasing biotite contenmarking foliation planes

223.1-223.9: GREY PEGMATITE226.0-229.3: SHEARED CHLORITIC GREY

WACKE-carbonate alteration alonifractures at 35 0 to C/A.

-chloritic alterationparallel to foliation at25 0 to C/A.

Siliceous Greywacke- fine grained with trace pyrite alongfoliat ion230.7-233.5: biotite along foliation

28" to C/A233.5: carbonate stringers.

233.5-234. 1234.5: garnets with increased235.4 biotite along foliation

237.0-238.9 planes.-garnets about 1/B" indiameter.

238.9-239.1: large garnets 1/4" Lo3/8" in diameter

HO

1

\ W l *H

'DES

S A M f ' i

f SQw

rF OOT A T, f

'0 101*1

ASSAYS

01 - tQn 01 t ot

\

\

j;'

DIAMOND DRILL RECORD NAME Of PHOPFRTY

,,mFNO MSL 86-5Massiye _Energy^L imited___ . - . our c t NO ——-————roo T A c; f:

,HO- TODESCRIPTION

-foliation at 30 0 to C /h-strong biotite association withthe foliation.239.6-241.5: stringers of quartz-carbonate247.0-247.3: quartz vein

247.7-248.5: PEGMATITE with 3% biotitephenocrysts248.5-258.0: becoming more siliceous withquartz phenocrysts.

250.0-253.0: slightly mineralized-34 pyrite-trace cerargyrite256.0-256.9: garnets with pyrite stringersparallel to foliation at 60"to C/A.

263.7-264.3: PEGMATITE - slightly potassic265.0: trace pyrite along foliation265.5-265.6: quartz vein with trace pyriteand small garnets.267.6-267.8: quartz- feldspar vein268.0

269.6: talc-chlori to alteration inthin vein.

-vein parallel to foliation at60 0 to C/A

274.2: CARBONATE STRINGER with tracepyrite parallel to foliationat 60" to C/A

-also fracture (at right anglesto foliation) filled withquar t z- carbonate

274.2-279.0: carbonate alteration in fracturiparallel to foliation277.5: quartz stringer

SAMPUE

HO.

8613

8613

!S

X Sui^w

.00

3

4

FOOTAGCrftOM

248.4

252.9

TO

252. ̂

258. (

TotM

4.5

5. 1

ASSAYS ,AU Aq-. O l to*

Tr

Tr

01 TOM

Nil

Nil

|

1

DIAMOND DRILL RECORD NAME OF PROPERTY.

HOLE n o. .-MBL 86-5

Massive Energy Limited

SMEE T NO..TOOT AGE

r BOM

323.5

326.9

339.7

341.7

358.8

TO

326.9

339.7

341.7

358.8

362.2

DESCRIPTION

322.2-323.5: PEGMATITE

Biotite Greywacke - trace pyrite

Mineralized Sheared Greywacke - 104 pyrite, trace agrentite- sections with garnets and chloritic altera tion- talc and chloritic fractures parallel tofoliation- foliation at 70 0 to C/A330.7-338.0: garnetiferous - more siliceous

- trace argentite- pyrite parallel to foliation@ 70 0 to C/A

339.0: trace argentite

Biotite Greywacke- foliation at 70" to C/A

Siliceous Greywacke- phenocrysts at quartz - trace pyrite along foliation @ 70 0 to C/A- zones of chlorite alteration along fract ures parallel to foliation

347.7: quartz carbonate alterationin fractures

349.0-350.0: garnets 1/8" in diameter -25i350.0-358.8: biotite shards along foliationat 60" to C/A

- trace pyrite- trace garnets at 358.0 feet.

Pegmatite - slightly potassic 360.8-361.0: chloritic biotite grey-361.4-361.9 wacke with foliation at

70" to C/A

SAMPLE

MO

S613

J613 5613

8614

8614

a iui'H toe s

j

i )

0

1

FOOTAGEfVOw

323.8

326.5 331.9

338.0

343.0

10

326.5

331.9 338.0

343. (

348. (

'01*1

2.7

5.4 6.1

5.0

15.0

A!Su- YS Ag•\ of. lot

Nil

0.03Tr

0.03

Tr

b t TO*

Tr

17.33 14.6*

11. 2 f,

Nil

DIAMOND DRILL RECORD NAME O F PROPERTY——..,~. ,. ..~ MBL 86-5

Massive Energy Limited

SHEET NO. .FOOTAGE

r ROM

362.2

370.5

371.0

387.4

TO

370.5

371.0

387.8

405. 4

DESCRIPTION

Sheared Greywacke- biotite rich greywacke with biotite alonefoliation at 70" to C/A- becomes more sheared with increasingchloritic alteration toward mineralized area.

Mineralized Greywacke- mineralized section between shearedgreywacke and garnetiferous greywacke- very siliceous with quartz crystals edge:and between tiny fractures- 2% PYRITE- 'H ARGENTITE- some biotite porphyroblasts evident

Siliceous Greywacke- foliation at SO 0 to C/A- very siliceous - fine to medium grained371.0-375.3: garnets up to 1/8" ; 20%

distributed equally through out section

- some shearing evident175.3-175.6: SHEARED PEGMATITE

- continuation of garnets from375.3 ft. to 375.6 ft.376.6-376.7: quartz-carbonate stringer at25 0 to C/A

- foliation at 40" to C/A379.6-381.5: beds of short shearedchloritic sections withquartz ve i ns .

Sheared Siliceous Greywacke- fine to medium grainjd. More shearedthan previous section.387.8-389.3: garnetiferous with chloritic

alteration

SAMPLE

wo

86148614

8614

861.

861

X SUl*M

23

4

5

6

364. 0368.8

372.8

382.0

387.0

FOOTAGE

368.372.

376.

387.0

390.5

i 4. 7i 4.0

7 3.9

5.0

3.5

*KVf ys Ag-. i or row

TrTr

0.03

Tr

T r

bf TON

Nil17. 11

9.77

Nil

Nil

DIAMOND DRILL RECORD NAME OF PROPERTY Massive Energy Limited MOI.E NO MBL 66-5—-—-————— SHEET NO.____;

FOOTAGE

r now

405.4

414.5

TO

414.4

444.5

DESCRIPTION

-mineralization is massive - 15%-and follows foliation at 60 0 toC /A

389.3-392.4: short fine garnet sections atapproximately 1 ft intervals

-some chlorite alteration392.4-393.3: MINERALIZED ZONE

-301 garnets with 1/8" diameter15t pyrite along fractures

402.0-403.3: SMALL MINERALIZED ZONE-5% garnets-21 pyrite stringers parallel tofoliation

403.3-405.4: fine grained garnets

Pegmatite- slightly potassic- contacts at both ends contain more siliceoigreenish quartz for 4".

Silicieous Sheared Greywacke- trace pyrite along foliation414.5-415.4: garnets with pyrite stringers

(31) parallel to foliationat 60" to C /h.

416.3: quartz vein at 70" to C/a416.3-416.8: garnetiferous mineralizedshear zone

- garnet porphyroblasts 1/4"diameter

- 4* pyrite417.6-418.0: chlorite alteration429.8-430.1: mineralized along foliation at

30 0 to C/A- chloritic with 5t PYRITE

437.1-438.0: sheared quartz vein

SAMPLE

NO

1614

3614

s

8614

861! 861!861!861!

•XHM'K

IOC!

'

i

9

0 123

i

fOOTAGErftow

390.5

400.0

414.4

425. 7 430.2434. 1438.0

10

394.8

405. .

418.

430. 2 434. 1438.0443.0

lOML

4.3

5.3

4.0

4.5 3.93. 95.0

AAtfYS Aq

i

1 i

01. TON

Tr

Tr

T r

TrTrTrTr

til TOW

Nil

Nil

i

Nil

NilNilNil

1.41

DIAMOND DRILL RECORD NAME OF PROPERTY Massive Energy Limited^HOI F NO MSL 86-5________________ SHEET NO 9

FOOTAGE

r ROM

444.5

445.1

447. 3

to

445.1

447.3

459.8

DESCRIPTION

438.8-439.5: 31 PYRITE, and garnetsparallel to foliation at 50'C/h

439.9-440.0: quartz vein at 40 0 to C/A440.0-443.1: garnetiferous and sheared

Pegmatite- trace .garnets- biotite inclusions at 10" to C/A

Biotite Greywacke- strong biotite at 40" to C/A and paralic

to foliation- quartz-carbonate stringers along foliat:

plane.

Sheared Siliceous Greywacke- chloritic sections- foliation at 60 0 to C/A

451.0: quartz veins452.0

450.0-450.5: sheared and chloritic450.5-459.0: increasing amount of

biotite shards parallel Lofoliation at 60" to C/A

459.0-459.8: quartz and fine dissemin ated pyrite along foliation

- also along fractures atright angles to foliation

459.8-466.0: trace small garnets463.4-470.0: sections almost completely

silica duo to silica flood ing. Follows remnant bedsparallel to foliation.

- foliation at 60" to C/A.470.0-472.0: increasing biotite along

foliation.

SAMPLE

NO

1

on

861!

861!

861

\ lUl'M

IOCS

4

5

5

FOOTAGErnOM

454.0

458.0

461.0

10 101*1

i

458.0

461 .0

466. 0

4 . 0

3. 0

*ftlT* Ag

1."

l5 . 0 j

i

i

\ 01 ro*

Tr

Tr

Tr

tit T ON

i

1

Nil

Nil

Ni 1

1

DIAMOND DRILL RECORD NAME OF PROPERTY Massive Energy Limited MOLE NO. __MSL 86-5______ SHEET NO 10FOOT AGE

r ROM

459.8

500.0

TO

500.0

DESCRIPTION

Siliceous Greywacke- very siliceous- biotite and sericite parallel to foliatiorat 30" to C/A

488.0: foliation now at 50" toC/A

490.5-490.9: sheared494.6-495.2

496.1-496.2: trace garnets 1/8" diameter496.5-498.6: very siliceous sections as in463.4-470.0 ft.498.6-498.9: quartz-carbonate vein at 60"to C/A and parallel tofoliation.

498.9-500.0: rich in silicaEnd of Hole

l^ti W43-

Peter EitutisMarch 30, 1986

SAMPLE

"0 \ SUL'N,

lOt!F DOT AGt

rnoM TO tOI*i

ASSAYS

-.

'

01 r on bf ton

1

i

'

DIAMOND DRILL RECORDNAME OF PROPERTY Massive Borland Lake________MBL 86-6 , C kl ^ TU 340 feet

-bpc- MJSH MIOT COW-OKA TION INC.

HOLE NO.

LOCATION

LATI TUOE

ELEVATION

LENGTH

Borland Lake GridLO+50E DEPARTURE 1 + 75S

004". AZIMUTH

STARTED March 28. 1986____ DIP

March 29. 1986

FOOTAGE

340

DIP

-37"

AZIMUTH

004"

FOOTAGE DIP AZIMUTHHOLE NO. 66-6 SHEET NO. __i.

REMARKS Casing pulled

LOGGED BY Konnpfh w,FOOTAGE

FROM

0

57.0

67.0

r

TO

57.0

67.0

111.4

DESCRIPTION

Casing in Overburden

Greywacke - fine grained with a slight foliation at irregular angles; strongly dragfolded along core

axis with slight carbonate alteration associated with brecciated sections; trace pyrite along fracturi planes.

Biotitif erous Greywacke - moderate foliation at 50" to C/A with204 biotite phencrysts marking foliation planes;

good silicification evident; trace very fine grained pyrite evident along foliation planes; some sections brecciated with weak carbonatization associated.71.0-72.4: Pegmatite 72.9-73.3: brecciated and dragfolded

section with weak carbonatealteration.

78.3-79.0: broken/ground core. 80.0-86.0: Trace to H pyrite 85.6-86.0

86.7-87.8: 3% pyrite in irregular string ers associated with biotite-rich zone; trace Marcasite.

88.0-89.2: White Pegmatite 89.5-89.791.3-91.6: brecciated greywacke zone with 92.1-92.8 slight carbonate alteration.

SAMPLE

NO.

86H

•MM -

7 34

FOOTAGEFROM

85.0

ro

88. 0

TOTAL

3.0

A fcfi A VA\

v i; OZ/TON

T r

02/TON

Ni J

l

DIAMOND DRILL RECORD NAME OF

MOLE NO.Massive Bo r l and, kak.e.

SHEET NO.___zFOOTAGE

f ROM

111.4

128.3

TO

128.3

142.4

DESCRIPTION

103.4-104.2104.5-105.1: White Pegmatite

108.1109.1-109.6

Siliceous Greywacke- slightly to moderately siliceous andfine grained; slight foliation at 60" to C/A; finegrained biotite shards mark the foliation planes.

112.0: weak stringer of pyritein sheared and siliceoussection.

115.7-116.8: siliceous Pegmatite; near t tselvage.

125.0-127.0: siliceous greywacke becomesmoderately sheared withsiliceous, angular porphy-roblasts evident in a finegrained siliceous matrix.127.8-128.3: sheared and chloritic grey wacke with a strong foliat ion at 60" to C/A.

Garnetiferous Greywacke- sheared and highly bioti tiferous grey wacke with sections exhibiting up to20% garnet porphyroblasts up to 1/4"in diameter; strong foliation at 65" toC/A; up to 54 disseminated pyriteassociated with the garnetiferous sect ions.135.2-136.1: 20% garnet porphyroblasts

with 5% stringer pyrite.137.2-137.4; White Pegmatite.138. 2-139.2

SAMPLE

MO.

861!861!86K

\ SUl'H

ID(S

890

FOOTAGEJ*0"

127.0132.2134. 4

ro

132.2134.4137.0

Torit

5.22.22.6

l

ASSAYSa n irt

x o* TD*

TrTrTr

' ' j ——01 TOM

Nil iNilNil

DIAMOND DRILL RECORD NAME OF PROPERTY,

HOLE NO. __MBL R6-Borland-Lake^

SHEET NO. . -3.TOOT AGE

r BOM

142.4

143.1

153.5

176.2

196.2

*

TO

143.1

153.5

176.2

196.2

208.;

DESCRIPTION

Pegmatite Dyke- white pegmatite with sericitic selvages

Siliceous Greywacke- very siliceous greywacke, massive toslightly foliated and black; grades into opaquelysiliceous section carrying Trace to 14 finelydisseminated pyrite along foliation planes at 144.0148.5-148.8: Pegmatite selvage.150.0-151.0: broken core.

Greywacke- finely bedded to sheared over shortsections; trace pyrite along fracture/foliationplanes.167.7-168.9: Pegmatite171.2-172.2: siliceous/sheared section

with 104 pyrite inirregular stringers.

Mineralized Greywacke- highly sheared and silicified zone withsheared and chloritic contact zone at 176 feet;strong foliation at 30 0 to C /h especially in biotite-rich sections; good sulfide mineraJ ization through out in disseminations and irregular stringers; 101total sulfide throughout core length: 54 stringerpyrite, 34 argcnti te/galcna , 2?, sphalerite inirregular masses.

185.0-186.0: 34 sphalerite187.0-188.0: up to 54 argent i tc-galena

mixture.

Potassic Pegmatite Dyke- megacrystic with trace pyrite alongfractures.

SAMPLE

NO.

86168616

86K861f86K86K86K86K8611861861861

l SULPM iOCS

12

34567890'l2

FOOT ACEf*OM

141.0143.0

171.5172.5176.0182.0187.0192. 3196.3208.0212.0217.0

TO

143.148.

172.5176.0182.0187.0192.3196. 3208.0212.0217. 0220.0

TOT4L

) 2.01 5.0

1.03. 56.05.05.34.0

11.74.05. 03.0

ASSAYSAn An

*. 01 TO*

TrTr

TrTr

0.010.010.030.03TrTr

0. 050.06

——— -J ———

01 TOM

NilNil

NilNil18.4319. 35j26. 2910.95NilNi 19. 6i

21 . 1C

11.4

J

/4/i

DIAMOND DRILL RECORD NAME OF PROPERTY Massive Bor]and,Lake, MBL 86-6

.————^-———-——.-.___.... '.MEET H O. ^__MOLE NO. .

root ACEf MOM

208.0

234.6

243. 3

306.5

TO

234.6

243. 3

306. 5

340.0

DESCRIPTION

Greywacke- finely bedded greywacke with a moderatefoliation at 60" to C/A; some sheared sectionsexhibit chloritic and carbonate alteration.214.3-218.1: sheared and siliceous

section with 2% disseminatetpyrite; 11 argentite/galena

236.0: Pegmatite.

Siliceous Greywacke- as previous; clots of disseminatedsericite throughout.

Biotitif erous Greywacke- strong foliation with 101 to 15% biotitishards marking foliation planes; strong foliationat 25" to C/A.248.8-249.8: contact zone with pegmatite

dyke; 10% pyrite withoccasional garnet porphy roblast.

249.8-251.7: Potassic Pegmatite Dyke258.0-260.6: sheared and carbonaceoussection with 2 1 pyrite instringers .

270. 7-272. 7274. 0-276.7277.3-278.7: White Pegmatite Dyke.279. 1-279. 8282.0-282.9

287.0: stringer of argentite 1/8inch in width.

- at 290.0 feet foliation is at 35 0 to C/Siliceous Greywacke

- as previous with slight foliation at

SAMPLE

NO.

8611861'

861"

861'

^-

1 lUl*"

IO(S

34

5

6

FOOTACtf *OM

247.0251.7

257.0

286. 0

10

251.7253.7

262.0

288.0

'01*1

4. 72.0

5.0

2.0

ASSAYSAn An

l 01 TO*

0.07Tr

Tr

Tr

b t TO*

23.38Nil l

Nil

Ni l

DIAMOND DRILL RECORD NAME OF PROPER TV Massive Borland LakeHOLE NO. . MBL 86-6 _ ^ SHEET

TOOT AGE

r MOM TO

340.0

DESCRIPTION

40" to C/A.312.5-313.0: chloritic shear zone317.3-317.6: siliceous shear zone. 319.1: quartz-carbonate vein at 50" to C/A; 20% pyrite associatec

width 1/4 inch.321.4: fracture at 50" to C/A with

trace argentite.326.2-327.2: sheared and garnetiferoussection with banding at 60"to C/A; hematite alongfractures parallel tofoliation; vuggy quartzcarbonate stringer evident;trace argentite.331.2-332.0: quartz-carbonate vein withsericitic alteration alongselvages.

- bedding at 45" to C/A evident.

End of Hole

Kenneth W/ JohnsonMarch 29, 1986

SAMf'LC

..0

8617 8617

\ lUL^H

iocs

7 8

f DOT *CCr •O 4'

318.0 323.0

'o

323.1 328.

IOt'1

) 5.0 3 5.0

ASWS Ag-. i oi - ron

0.03 Tr

b l T DK

0. 87 Nil

;r1

FELSIC INTRUSIVE ROCKS

Pi Pink PegmatiteP; While PegmatiteAi ApliteGc Sheared Granite, Feldspar Augen Gneiss

Si Granite

MAFIC AND ULTRA MAFIC INTRUSIVE ROCKS

60 Diorite 6b Gabbro

6c Peridotite

CHEMICAL METASEDIMENTS

5a Chert

5b Limestone5c Oxide Facies Iron Formation5d Sulphide Facies Iron Formation

l 4 j CLASTIC METASEDIMENTS

4a Quartzite

4b Siliceous Metagreywacke4c Metagreywocke

4d Argilite

4e Sericitic Metagreywocke

4f Sillimanite Schist

4g Tuffaceous Sediments

FELSIC VOLCANICS

3o Flows

3b Tuffs

3c Lapilli Tuff3d Agglomerate3e Cherty Tuff

INTERMEDIATE VOLCANICS

2o Flows

2 b Tuffs2c Lapilli Tuff2d AgglomeroTic Tuff

MAFIC VOLCANICS

lo Undifferentioled Flows

Ib Medium Groined Flowsle Pillowed Flows

Id Amphibolitized Volcanic

le Tuff

SYMBOLS

Area Of Bedrock Outcrop

Bedding, Strike And Dip

Foliation, Strike And Dip

Joint Ptone

Fault With Displacement

Shear Zone

TIE LINE 15 N

5N

BASE LINE 00

5 S

10 S

Borland L oke

LEGEND

SHEET LAYOUT

WEST

l

EAST

BUSH PILOT CORPORATION

Massive Energy/Noranda Option BORLAND L AKE PROJECT, ONTARIO

PLAN OF DIAMOND DRILLINGWEST SHEET

SCALE 1":100 FEET APRIL 1986

ANADA

Dwg. No E.'C.

53D16NEa084 63.4856 BORLAND LAKE S00

B o r l a n d L oke

BASE LINE 00097 D )

10 S

BUSH PILOT CORPORATION

Massive Energy/Noranda Option BORLAND LAKE PROJECT. ONTARIO

PLAN OF DIAMOND DRILLINGEAST SHEET

SCALE 1":100 FEET APRIL 1986

TDRQNTO CANADA

Dwg. No E.I.C

Q/fl

53D16NEM84 63.4856 BORLAND LAKE 210

3s d

TIM

IM3M

7 M

—

.4—-

1 to

S3D16NE0004

63.4856

BORLAND

LAKE

r

i ^n an

*ii.

.

O1

IMIM

-—-..

.,3

!IM

UV7SC - i

L2

if. IM

OO

1 to

\

p

53D16Nee004

63.4856

BORLAND

LAKE

230

v- -

---"*

- ni

r if-

*- f

*'

IM•j

,*^

ai.

iii.

^- i

t-^

i

3'IM

ara

SIM

e1 M

\

L2

36-'V

2-

+Z5E

x

3*^0

53

0 oo

-V-

At.

o-o

h O

'.A

"X.

53D

16N

E00

04

63

.48

56

B

OR

LAN

D

LAK

E2

40

•l—

*li

-W-J

—

*-.

'

1 to

.***^n

riQ

ST

?

-

J...^

&JF-

"' : ;r

l

I'M

IMai

\iS4

\l

1 to

53D

16N

E0I

B04

6

3.4

85

6

BO

RLA

ND

L

AK

E2

50

V

260

*-

Jjt:

roUJ UJ

roUJ10

UJ LUr-

UJ CO

UJen

SL Lake Level

100 L

200L

300 L

400 L

65-27V?

65-1995

•i

BLOCK 'A

53016NEOei84 63.4856 BORLAND LAKE

270

In com p l e t e

Drilling

29V

Water

Lacustrine Clay

23

Incomplete

Drilling

65-9

BLOCK 'C

MASSIVE ENERGY LTD.BORLAND LAKE PROPERTY - ONTARIO

VERTICAL LONGITUDINAL SECTION

BLOCK 'B 1

A GGRADE-THICKNESS CONTOURS

40 8O l 2O 160

FE ET

D. A. Bourne, K.W.Johnson April , 1986

O

IOOL

200L

300 L

400 L

500 L

ro

o"

3,875 8- 66, 0-03

65-27

53DI6NE0004 63.4856 BORLAND LAKE

O6S-/9

4,1676'66,0-03

o 8

3,0839-44 t O-OI

BLOCK 'A 1

Incomplete

Drilling

X-RAY 2O

10,91711-83,0-03

29

85-3

23,2921310, O 03

85-1

X-RAYI O

29,0838-96,0 03

65-18

65-4

85-2

46,10012 93,0-02

65-2

LU

69,1677 87, O 01

^ 9

65-l

28

LU OJ

55-3

28,875911 , TR

65-14

15

20,1259-91,0 01

23,0416-01 , TR

86-5

O86-4

Lacustrine Clay

LJ m

LJ iuin

LU(D

LJN

LU GO

Lake LevelWater

O10

65-tl

22,8753-92,0 O

27

65-15

36,6666 74, TR

37,2327-07, 0-01

26

O86-1

86-3

BLOCK 'B 1

55-5O

20,27111-28,0 04

55-5

14 O

6,937619,O 08

65-7

8,6045-60,0-07

86-2O

Incomplete

Dri M ing

LEGEND

8 O-

2,083-9-44,0-01

-MINERAL INVENTORY BLOCK

D.D. HOLE NUMBER

PIERCE POINT OF D.D.HOLE

-TONS

-oz Ag , oz Au

65-16 O

2,0833 52 .0-01

5,4165-50,0-02

23

25,0004 66, 0-O3

55-5

17

6,1587-92,0 12

25

65-9

BLOCK 'C 1

MASSIVE ENERGY LTD.BORLAND LAKE PROPERTY - ONTARIO

VERTICAL LONGITUDINAL SECTION GEOLOGICAL MINERAL INVENTORY

400 l

800 200 i

1600

FE ET

D A. Bourne, K.W.Johnson April , 1986

u en

\

63.4856 BORLAND LAKE 230

LEGEND

Interpreted fault showing basis for projection .. . ..

M - Magnetics V - VLF EM (NAA)

Projected geologic contact

AEM conductor axis... ...

Ultramafic intrusion or plug

BUSH PILOT CORPORATION

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO

ELEMENTS OF STRUCTURE

SCALE 1:10,000 MAY 1986

EXCAL1BUR INTERNATIONAL CONSULTAMTS LTD.

TORONTO, CANADA

Dwg, No. E.I.C.- 1678

in rO rO

rOro

oo rO rO

OrO

5SOJ

CO OJ

?(M OJ

in OJ OJ

rO OJ

OvJ

OJ OJoOJ 00 ro Osi O

t C', , 4500NTIE LINE 15 N

10 N

BASE LINE 00

5 S

10 S

B or l a nd

ic'2 ,3700SL oke

SHEET LAYOUT

EAST

LEGEND

Instrument: Rx-Huntec Mk IV, Tx-Phoenix 1PT-1 Electrode configuration: Gradient array, 0 = 100' Chargeability contour interval....... 5 msecs25msec contour. 5 msec contour. De press ion.......

BUSH PILOT CORPORATION

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO

CHARGEABILITY CONTOURS Gradient Array

WEST SHEETSCALE 1^100 FEET APRIL 1986

Dwg. No. E.I.C-I679A53DI6NE0B04 63.4856 BORLAND LAKE

300

t C,,4300N

BASE LINE 00(Bearing 097 0 }

B o r and L okeT C 2 ,4200S

BUSH PILOT CORPORATION

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO

Instrument: Rx-Huntec Mk!V, Tx-Phoenix IPT-1 Electrode configuration: Gradientarray.a =IOO Chargeability contour interval....... 5 m sees25msec contour 5msec contour. Depression

SHEET LAYOUT

CHARGEABILITY CONTOURS Gradient Array

EAST SHEETSCALE 1=100 FEET APRIL 1986

Dwq. No. E.I.C-I679B53D16NEC0&4 63.4856 BORLAND LAKE

m ro ro

ro rO

CO PO

OrO

O CO

CO CO

h- oo

toCNJ

toC\J (\J

roCO

CM CO CO

oCJ

tCO r- rO OJ O

Ci, 4500NTIE LINE 15 N

BASE LINE 00

5 S

10 S

B o r l Q n d

|C'2 ,3700SL oke

SHEET LAYOUT

WEST EAST

LEGEND

Instrument: RxHuntecMk IV ,Tx- Phoenix l PT-1 Electrode configuration: Gradient array,a z IOO' Contours of apparent resistivity int. lOOOflm 5000am contour. 1000 firn contour. Depression ........,....100 a 200Urn contours within anomalously low domain.

BUSH PILOT CORPORATION

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO

RESISTIVITY CONTOURS Gradient Array

WEST SHEETSCALE 1"-100 FEET APRIL 1986

Dwg. No. E.I.C.-1680A53D16NE00IB4 63.4856 B ORLAND LAKE 320

4 C,,4300N

TIE LINE ION

BASE LINE 00

B o r land L okeC 2 ,4200S

BUSH PILOT CORPORATION

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO

Instrument; Rx-Huntec MklV, Tx-Pnoemx l PT-1 Electrode configurofion: Gradient array, a = Contours of apparent resistivity int.lOOOOm 5000 Jim contour 1000 Dm contour Depression .100 8r 200 H m contours within anomalously low domain

SHEET LAYOUTRESISTIVITY CONTOURS

Gradient ArrayEAST SHEET

SCALE 1=100 FEET APRIL 1986

Dwg. No. E.I.C.-I680B53D16NE6004 63.4856 BORLAND LAKE

LOro PO

rO PO

00rO rO

OrO

(T) 00

CO 00

r-CO

o?00

lO 00 00

ro 00

0000

o00 a.) r- U") •r rO CO

TIE LINE 15 N

5 N

BASE LINE 00

10 S J lil O

B or l on d L oke

SHEET LAYOUT

WEST EAST

LEGEND Instrument....... ........Gem Systems GSM-8Bose station.................,......CMG MR-10Total field base level.............. 59,000 nTContour interval........................... 50nT5000 nT contour.500nT contour.50 nT contourDepression.............................r"*

BUSH PILOT CORPORATION

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO

TOTAL FIELD MAGNETIC CONTOURS

WEST SHEETSCALE 1"^100 FEET APRIL 1986

53D16NE8004 63.4856 BORLAND LAKE 3-40 Dwg. No. E.I.CH68IA

00 (D ro c\JO O

UJ OJ

UJ

roUJ UJ

inUJ

(D

LJr-

UJ

CO

LJ

(D

UJ

OUJ UJ

CMUJ rO

UJ

inUJ UJ UJ

COUJ CD

UJ

oCM

B o r l an d L oke

SHEET LAYOUT

WEST EAST

LEGEND Instrument ................Gem Systems GSM-8Base station.......................CMG MR-10Total field base leveL............. 59,000 nTContour interval........................ 50 nT5000 nT contour,. 500 nT contour. 50nT contour Depression

BUSH PILOT CORPORATION

TIE LINE ION

5 N

BASE LINE 00

10 S

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO

TOTAL FIELD MAGNETIC CONTOURS

EAST SHEETSCALE 1"^ 100 FEET r APRIL 1986

53DI6NE0004 63.4656 BORLAND LAKE Dwg. No EIC.-I68IB3S0Q/7?

Zoneapprox. position only )

S o l o n Pon

BASE LINE 00

LTRAMAFIC

AFIC INTRUSION

f a n d L oke

BUSH PILOT CORPORATIONLEGEND

Mineral prospect, horizon......

Polarization axis of note .....

Polarization ring structure

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIO

Interpreted fault showing relative movement and basis for projection

M — MagneticsV - VLF EM (NAA)G — GeologyD — Drilling

SHEET LAYOUT

INTERPRETATIONWEST SHEET

Iron formation marker horizon

SCALE 1"MOO FEETProposed DDH with identification and horizontal projection

Geologic contact inferred ..

Postulated fold axis synclinal , anticlinal.

Dwg.No.E.I.C.I682A53D16NE0004 63.4856 BORLAWD LAKE

N0.86-G3

ETA VOLCANO -SEDIMENTARY DOMAIN

ULTRAMAFIC NTRUSION

So r land L oke

BUSH PILOT CORPORATIONLEGEND

Mineral prospect, horizon

Polarization axis of note .....^—

Polarization ring structure**"

Massive Energy/Noranda Option BORLAND LAKE PROJECT, ONTARIOInterpreted fault showing

relative movement and basis for projection

M - MagneticsV - VLF EM (NAA)G — GeologyD - Drilling

INTERPRETATIONEAST SHEETIron formation marker

horizor SCALE 1-100 FEETProposed DDH with ldent,fication and . horizontal projector

n —— -- No 86-G2Geologic contact inferred.... ——

Postulated fold axis synclinal, anticlinal

.r — — r —

Dwg.No. E.I.C I682B

370