davince tools generated shot-points were spaced at intervals of 1740 feet alongthe line and geophone...

COMMONWEALTH OF AUSTRALIA

DEPARTMENT OF NATIONAL DEVELOPMENT

BUREAU OF MINERAL RESOURCES, GEOLOGY AND GEOPHYSICS

\

PETROLEUM SEARCH SUBSIDY ACTS

Publication No. 19

QUILPIE-THARGOMINDAH-CHARLEVILLESEISMIC SURVEY, QUEENSLAND, 1959-1960

BY

PHILLIPS PETROLEUM COMPANYAND

SUNRAY MID-CONTINENT OIL COMPANY

Issued under the Authcrity of Senator the Hon. W. H. Spooner,Minister for National Development

1961

\ -.

COMMONWEALTH OF AUSTRALIA

DEPARTMENT OF NATIONAL DEVELOPMENT

Minister: SENATOR THE HON. W. H. SPOONER, M.M.

Secretary: H. G. RAGGATT, C.B.E.

BUREAU OF MINERAL RESOURCES, GEOLOGY AND GEOPHYSICS

Director: J. M. RAYNER

This Report was prepared for publication in the Geophysical Branch

Chief Geophysicist: R. F. THYER

FOREWORD.

In 1959, 'the Commonwealth Government enacted the Petroleum Search Subsidy Act1959, under which companies proposing to drill for new stratigraphic information or to carryout either geophysical or bore-hole surveys in search of petroleum could be subsidised for thecost of drilling or of survey operations approved by the Minister for National Development.

The Bureau of Mineral Resources, Geology and Geophysics is required, on behalfof the Department of National Development, to examine the applications, maintain surveillanceof the operations and in due course publish the results.

A seismic survey was carried out under the Petroleum Search Subsidy Act 1959in the Quilpie-Thargomindah-Charleville area of Queensland by Petty Geophysical EngineeringCompany for Phillips Petroleum Company and Sunray Mid-Continent Oil Company. ThisPublication deals with that survey and contains the information furnished by Phillips PetroleumCompany and Sunray Mid-Continent Oil Company"and edited in the Geophysical Branch of theBureau of Mineral Resources. The final report was written jointly by Mr. C. D. Hier. ChiefGeophysicist, Australian Operations, Phillips Petroleum Company and Mr. C. J. Spivey,Supervisor, Australian Operations, Pctty Geophysical Engineering Company. The methods ofcarrying out the seismic survey and the results obtained are presented in detail.

Plate

CONTENTS.

ABSTRACT

INTRODUCTION

GEOLOGY AND PURPOSE OF THE SURVEY

FIELD PROCEDURES

RESULTS OF THE SURVEY

METHODS OF COMPUTATION

INTERPRETATION OF RESULTS

CONCLUSIONS

REFERENCES

APPENDIX : Statistics

ILLUSTRATIONS.

I. - Location Map and Geologic Sketch Map ....

II. - Structure Contour Map on "Blythesdale"Horizon - Thargomindah area

IH. - Structure Contour Map on "Blythesdale"Horizon - Quilpie and Charleville area

IV. - Structure Ccntour 1\1ap on "Base ofMesozoic" - Thargomindah area

V. - Structure Contour Map on "Pre-MesozoicPhantom" - Quilpie and ChaTleville area

VI. - Cross-section of Traverse A-A'. Sheets 1 and 2

VII. - Cross-section of Traverse B-B'. Sheets 1 and 2

Page.

1

2

2

3

4

5

6

8

9

10

Frontispiece

At back ofreport

"

"

"

"

"

ILLUSTRATIONS. (Continued)

VIII. - Cross-section of Traverse C-C', Sheets 1 and 2

IX. - Cross-section of Traverse D-D',

X. - Cross-section of Traverse E-E', Sheets 1 and 2

XI. - Cross-section of Traverse F - F', Sheets 1 and 2

XII, - Cross-section of Traverse G-G'.

XIII. - Record Section of Traverse H-H'.

XIV, - Record Section of Traverse 1-1',

XV. - Record Section of Traverse J-J',

At back ofreport

"

"

"

"

"

"

"

LOCATION MAP a GEOLOGIC SKETCH MAPafter F W. Whitehouse

P - Permian

£0- Cambrian - Ordovician,Boulia Shelf.

pt- Pre Cambriari

Scale: (= 120 miles

..,.....,....., Edge of Mesoloic outcrop.Metamorphic rock on edge of basin

8 beneath Mesoloic.

+++++ Granite beneath Mesoloic.

~ Sub- Mesoloic structural basins. 40 0 40

kiJ'80 120

I =:!!l

'.', .:::.

ROCK~AMPTON•

ROMA

SURATSUB-BASIN

\p

Maps,Plates mavli>- Befoofo Plates II a J3[ .rl----....

S~A:I cl ~~-I-t---:-CH-A-Rl-EV-,l-l-ll'O~ «>r:v- QJ:!'"PIE ~ ~

~Cj \JQ,) ~-\'f.0 \ s I---+------l

. ATIP 72P ,'?~~l/nnom,ncko THARGOMINDAH . ; ~~;/!

o , \ CUNN~MULLA :~ I

+ _}- - - IQ:) :/1 J::....... ,~,

1- -r-+.w+;I " . ;. , '~ I

+ ,+ + '= EULO··':, :'.'

~_ QUEE;NSLA~D__:_ + 'gH~~F-···:.:-.·~.:-~.r:_·:.:.l_:·:'__

N.sW. + + +') '.+ ~ ~ I

I '+/,+',

.,".' :-.\

')\.:\+ + '~".~:,)+ + +':"

I+ + +,

+ + I

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: + "l\ I /V 1+." ',-"-v -,

BOULIA .--~I

S 'ELF ~/~~ .

25ol-..\.-------------t------------.:i..:o--/-~'---U~-

140 0 1500

Plate J.

ABSTRACT.

A reconnaissance seismic survey, subsidised by the Commonwealth of Australia,was made for Phillips Petroleum Company of Bartlesville, Oklahoma, D.S.A. and SunrayMid-Continent Oil Company of Tulsa, Oldahoma, D.S.A. by Petty Geophysical EngineeringCompany of San Antonio, Texas. This survey was located within Authority to Prospect 72Pin the Quilpie-Thargomindah-Charleville area of South-western Queensland.

The purpose of the survey was to obtain information on the regional geologybeneath the M.esozoic formations of the Great Artesian Basin north and west of the Eulo Shelf.Three deep structural basins beneath the sub-Mesozoic unconformity are indicated.

/

INTRODUC TION.

The seismic survey is located in Authority to Prospect (ATP) 72P in theQuilpie-Thargomindah-Charleville area of South-western Queensland, Australia.

The seismic work was done by Petty Geophysical Engineering Company of SanAntonio, Texas with Mr. Oliver McClellan as Party Chief. Other key personnel includedW. P. Le Croix, Party Manager; Ken Kallestad, Observer; Ross Smitherman, Surveyor;and Clarence Moore, Driller. Sixteen additional men completed the crew.

Topography varied from flat plains to rolling hills with brush and trees coveringmost of the area, but not sufficiently thick to require bulldozed trails for the reconnaissancesurvey.

Average elevation above sea-level was about 800 feet. Local relief rarelyexceeded 100 feet.

fhere were three field crew headquarters in towns (Quilpie, Thargomindah, andCharleville) and two in camp sites (Cooladdi and 20 miles north of Quilpie). The averagedistance from field headquarters to the working area was about 20 miles and the average roundtrip driving time was about 1~ hours.

The weather was generally clear and dry; however, the crew was unable to workon five days owing to rain.

The results of a previous seismic survey are also incorporated in this report.This earlier survey took about two weeks and was carried out near the town of Quilpie in June1958 by Foreign Oil Exploration, Inc. for Oklahoma-Australian Oil Company.

GEOLOGY AND PURPOSE OF THE SURVEY.

The Quilpie-Thargomindah-Charleville area lies on the eastern flank of theThomson Sub-Basin of the Great Artesian Basin. The known geologic framework of theQueensland portion of the Great Artesian Basin is indicated in Plate I, after Dr. F. W.Whitehouse (1954).

The surface geology is poorly exposed, the outcrop consisting almost entirelyof a surficial lateritic zone developed on the Cretaceous Rolling Downs Group. The siliceous"duricrust" zone of the lateritic profile is well developed in this area and caps most of theinterstream divides. The wide channels ofthe Bulloo, Paroo, and Warrego Rivers are flooredwith alluvial silt.

Deep water bores in the area indicate the presence of about 2500 feet maximumthickness of the Rolling Downs Group overlying a variable thickness of Blythesdale Group andsubjacent Jurassic and Triassic sediments. Seismic data indicate a maximum thickness ofabout 5000 feet for the total Mesozoic in the area. The "Mesozoic" section may includePermian strata as well.

2

The nature of the rocks underlying the Mesozoic sedimentary basin is unknownover most of the area. Granite ofDevonian(?) age is present in outcrop on the Eulo Shelf, andhas been penetrated at shallow depth in water bores in the same area. Slate and othermetamorphic rocks of unknown age are present in deep bores along the Nebine Ridge, whichseparates the Thomson and Surat Sub-basins.

Appreciable dips have been observed on the "duricrust" surface. For the mostpart the apparent gentle surface "structure" has no relation to structure mapped at shallowdepth seismically , and appears to represent an undulating ancient surface of erosion. Locally,however, dip in excess of 15 degrees is present where the "duricrust" surface appears to dipbeneath adjacent alluvial plains. One such structure at Mt. Constance was investigated with ashort seismic traverse (see Cross-section, Plate XII). No major surface anticlines such asthose mapped to the west by Santos geologists (Sprigg, 1958) are present in the QuilpieThargomindah-Charleville area.

The purpose of the survey described in this report was to investigate a thicksection of stratified rock unconformably underlying the Mesozoic. This thick section had beendemonstrated earlier in a short traverse shotthroughQuilpie in 1958 by Foreign Oil Exploration, Inc. It was also intended to investigate other possible areas of thick section north andwest of the Eulo Shelf, with a view to delineating potential "basins" of thick strata for localisingdetailed seismic work, and, eventually, determining a favourable location for a well to evaluatethe petroleum possibilities of the area.

FIELD PROCEDURES.

Equipment.

Vehicles (all International) used for the survey included two 6 x 6 RF-190 trucksmounted with Mayhew-1000 air-water drills, two 6 x 6 RF-190 trucks mounted with 1500-gallonwater-tanks, a 4 x 4 R-194 shooting truck mounted with 1000-gallon water-tank, a 4 x 4 B-120recording truck, a ten-passenger personnel carrier, and two pick-up trucks.

Recording equipment included a 24-channel SIE MS-15A magnetic recorder, anSIE DL-8 dual demodulator for making field play-backs, and Hall-Sears HS-1 geophones.

Shooting Techniques.

Most of the shooting was done with split-spread continuous profiling. Shot-pointswere spaced at intervals of 1740 feet along the line and geophone stations were 145 feet apart.From 4 to 32 geophones per station were used spaced 30 feet apart. Multipre geophone patternsused were as follows:

No. of geophones

4 to 81632

3

Pattern

In line"X"Parallelogram

A 20-90 filter setting was used as standard procedure on the magnetic tapes andalso on the play-backs. However, various other filter settings were tried for experimental andcomparison purposes.

Owing to variation of surface conditions in the area, optimum shot-hole depthsranged from 60 to 150 feet and charge of explosive from 2 to 30 pounds.

In some localities where it appeared that no pre-Mesozoic sediments are present,shot-holes were spaced 2 miles apart and reflections were correlated.

Experiments in recording were made using various shot-depths to 295 feet, shothole patterns of 2, 3, and 5 holes, multiple geophone patterns of 4,8,16, and 32 per trace invarious layouts, and a noise analysis study.

Drilling.

Two Mayhew-1000 drills. equipped for air or water drilling and mounted on6-wheel-drive International trucks, were used for shot-hole drilling. Two 1500-gallonwater-tanks, mounted on 6-wheel-drive International trucks, were used for supplying water fordrilling. Water was usually available from water wells, rivers, or creeks. Approximatelv 90%of the shot-holes were drilled with water and 10% with air.

Most of the drilling was in sand, clay, and shale; gravel and lignite wereoccasionally encountered. In some localities, drilling was difficult and rock bit consumptionhigh owing to a very hard layer of "duricrust", sometimes as thick as 30 feet, on or nearthe ground surface. One particular shot-hole required 10 hours drilling time and 4 rock bitsto penetrate this layer. During the survey one of the Mayhew drills was modified for airpercussion drilling and was then able to penetrate 30 feet of duricrust in about one hour, thussaving a great deal of drilling time and many rock bits.

Surveying.

Horizontal and vertical control were obtained by alidade and plane table and, ina few cases, by transit. Bench marks, astronomical points, and landmarks such as fences,roads, creeks, trees, bores, etc. were tied in while making the survey. Vertical closuresalong traverse were accurate within 5 feet and horizontal closures were made with a minoramount of error. Magnetic declination in the area averaged about 7t degrees east of truenorth.

RESULTS OF THE SURVEY.

Presentation of Results.

The results of the seismic survey are presented with this Publication in the formof contour maps, plotted cross-sections, and record sections.

The following additional data have been filed with the Bureau of Mineral Resources,Geology and Geophysics, and are available for future reference:-

(i) Complete set of plotted cross sections;(iI) Complete set of record sections.

4

Record Quality.

Record quality varied from good in the river flood plains to practically unusable insome of the "duricrust" areas. To ensure optirr..um record quality it was necessary to confinethe traverse lines to flood plains and valleys as much as possible. This resulted in somecrooked lines, but the sacrifice of straight lines appeared justified in these cases by theimproved record quality.

Record quality was usually improved when multiple shot-holes and multiplegeophones were used. However, this resulted in a loss of ground coverage, and, in manylocalities, the improvement in record quality did not appear to justify the use of rr..ultipleshot-holes, or multiple geophones in excess of eight per trace.

The data used in the sub-surface structure maps are considered generallyreliable.

METHODS OF COMPUTATION.

Up-hole times were used for weathering corrections, and data were corrected forelevation differences to a datum of+600 feet using an elevation velocity of 7000 feet per second.A "t.~t" analysis served to establish a velocity curve for the Mesozoic reflections conformingto the formula V = 5700 + 5Twhere V equals average velocity in feet per second and T equalsone-way time in mi.lliseconds. The limited~t information from pre-Mesozoic sediments wasnot considered sufficient to establish reliable velocities; however, it appears that these velocities are approximately 16,000 to 18,000 feet per second.

At reflection time of 1. 200 seconds (one-way time of 0.600 second) the averagevelocity was calculated to be 8700 feet per second. This reflection time, in terms of depth, wasnear the pre-Mesozoic unconformity in the structurally lowest localities, and was chosen as thevelocity for spacing of shot-points, Le. 1740 feet between shot-points divided by 8700 feet persecond equals 0.200 second. The cross-sections were thus constructed with one centimetrehorizontally representing 0.050 second, and one centimetre vertically representing 0.050second one-way time or 0.100 second two-way time.

Data were plotted in time on cross-sections and migrated by time resolution. Bythis method, shot-points are spaced on the sections with the horizontal scale nearly the sameas the vertical scale. Time data plotted below the shot-points are then swung in arcs from thedatum plane. Tangents to the arcs from connecting data are drawn to position the reflectinghorizons. Reflection times, however, are written directly under their respective shot-points.

The "t,At" analysis indicates that interval velocities inpre-Mesozoic sediments(16,000 to 18,000 feet per second) are much greater than interval velocities in the Mesozoic.Pre-Mesozoic reflections, therefore, are deeper vertically relative to the horizontal distancethan they appear on the plotted cross-sections.

5

INTERPRETATION OF RESULTS.

The correlated reflection event contoured on Plates 11 and III as the "Blythesdale"horizon is believed to be near the base of the Juro-Cretaceous Blythesdale Group. The "Baseof Mesozoic" horizon contoured on Plate IV is immediately above the assumed base of theMesozoic rocks. The "pre-Mesozoic Phantom" horizon (Plate V) is a phantom horizon beneaththe sub-Mesozoic unconformity.

It is assumed that the major angular unconformity at roughly 3000 to 5000 feetbelow datum where deep reflections were obtained represents the base of the Mesozoic. Inareas where consistent reflections below this depth were not obtained, it is assumed that theMesozoic rests on granite or metamorphic basement.

Thargomindah Area. (Plates 11 and IV.)

Correlation shot-points in the Thargomindah area were spaced at two-mileintervals except for three miles of continuous profiling near Thargomindah on Line 201,and six miles near Mt. Constance on Line 204, where a surface structure is indicated onthe "duricrust". Little or no reflection energy was obtained .from below the Mesozoic inpreliminary shooting; therefore, two-mile skips were made to speed an effort to locatepre-Mesozoic sediments. Reflection indications from depths below the Mesozoic werequestionable throughout the Thargomindah area, however, which suggests that pre-Mesozoicsediments are not present along the line worked in this survey.

The two contour maps, "Blythesdale" and "Base of Mesozoic", are based onlimited but fairly reliable correlations and show similar structure.

General north-west dip is shown in the eastern and central part of the area, witha structural nose or possible closure indicated at Shot-point 376, Line 202, and a broadstructural nose indicated along Line 203 about twenty-two miles south-west of Thargomindah.

To the west, a synclinal axis is suggested near Shot-point 322 by the higherelevation of the mapping horizons at Shot-point 327, Line 201. On similar grounds, anothersynclinal axis is suggested near Shot-point 402 by the data at Shot-point 405, Line 203. Analternative interpretation, however, could show the high points up-thrown by faulting.

A fault is indicated (see Plate XII) in the south-western part of the area on Line204 between Shot-points 410 and 411 near Mt. Constance. The throw of this fault appears to beabout 500 feet with the down-thrown side to the east. It corresponds to a narrow zone of steepeasterly dip in "duricrust" which forms the eastern flank of Mt. Constance Dome, noted on anunpublished photo-geological map of the Bulloo Quadrangle prepared by Geosurveys, Ltd.

Quilpie Area. (Plates III and V.)

Continuous profiling was used in the Quilpie area except from Shot-point 99 to 106on Line 1 where correlation shot-points were spaced at two-mile intervals. Reflections frompre-Mesozoic horizons were observed over an area extending north-south approximately 45miles and east-west approximately 20 miles, centred about 10 miles east of the town of Quilpie.Eastward from Shot-point 58 on Line 1 and eastward from Shot-point 128 on Line 4, onlyquestionable reflection events were observed from pre-Mesozoic sediments.

6

The structure contour maps on the "Blythesdale" and the "pre-MesozoicPhantom" in the Quilpie area (Plates III and V) are believed to give reliable representationsof the general regional structure. The pre-Mesozoic phantom horizon is about 2000 feet abovepresumed basement.

A synclinal axis trending north-south about three miles east of Quilpie is shownon both the Mesozoic and pre-Mesozoic phantom horizons (see cross-section on Plate VI). Amajor angular unconformity is established at the presumed base of the Mesozoic. Structuraldip ratio between the Mesozoic and pre-Mesozoic sediments is about 1:20.

o Pre-Mesozoic sediments truncated at the unconformity have steep east dip ofabout 35 from a point about one mile w~-st of Quilpie to the axis of the syncline, where theyreach a thickness of about 13,000 feet. It is inferred that granite basement is presentimmediately beneath the unconformity in areas where reflections were not obtained below theMesozoic sediments.

Three anticlinal axes were crossed within the Quilpie structural basin. Oneoccurs 13 miles south-east of Quilpie centred on Shot-point 862, Line 11, and has about 4,000feet of structural relief on this line (see cross-section on Plitte VII,Sheet 1). A secondanticlinal axis about 7 miles north-east of Quilpie, with its crest at Shot-point 447, Line 9,has about 700 feet of structural relief on the "pre-Mesozoic Phantom" horizon (see crosssection on Plate IX and record section on Plate XIII). A third anticlinal axis is indicated 15miles north of Quilpie on Line 4 (see cross-section on Plate VIII, Sheet 1). Further workwould be necessary to determine whether these features are structurally closed and alsowhether they have sufficient pre-Mosozoic section at their culmination to provide a satisfactory drilling prospect.

Four lines in the Quilpie area (F1, F2, F3, and F4) were shot by Foreign onExploration, Inc. Shot-point numbers for these lines are preceded by the letter "F" on allmaps in this report.

Charleville Area. (Plates HI and V.)

The seismic survey in the Charleville area consisted of shooting along ageneralised ~ast-west line about fifteen miles south of Charleville and extending from theeastern boundary of ATP 72P westward for approximately ninety miles. Also included isabout 16 miles of line north of the village of Cooladdi. Continuous profiling was used wherepre-Mesozoic reflections were obtained. In areas where only questionable pre-Mesozoicreflections were indicated, two to ten-mile traverse skips were made.

The "Blythesdale" and "pre-Mesozoic Phantom" maps are believed to givereliable representations of the general regional structure.

In the vicinity of Cooladdi a structural trough, which trends from north-west tosouth-east, is shown on both maps with structural relief in the ratio of about 1 :20 (see crosssection on Plate X, Sheet 2). The pre-Mesozoic trough is shown to be about eighteen mileswide, bounded on the south-west by a fault down-thrown to the east, with apparent displacementof 10,000 feet or more (see cross-section on Plate X, Sheet 1). Steep dip, or a fault with about500 feet displacement, is shown here in the Blythesdale Group. It is inferred that pre-Mesozoicsediments have been' removed by erosion west of the fault where true reflections do not

7

appear to exist below the Mesozoic.eastern flank of the Cooladdi trough;at the synclinal axis.

oSteep sOl.).th-west dip of about 30 is shown on the north-the pre-Mesozoic sediments thicken to about 16,000 feet

About fifteen miles south of Charleville, in the vicinity of Westgate, anotherstructural trough trending in a north-south direction is shown on both maps (see cross-sectionon Plate XI). The pre-Mesozoic trough is about sixteen miles wide, with steep flanks on eitherside. Pre-Mesozoic sediments are estimated to be about 10,000 feet thick at the axis of theWestgate trough.

In addition to the unconformity at the base of the Mesozoic, another majorunconformity, within the pre-Mesozoic sediments, is indicated at several places in theCharleville area. An anticlinal axis is indicated in sediments below this deeper unconformity(at about 12,000 feet in depth) at Shot-point 798 on Line 109, about eighteen miles south-westof Charleville (see cross-section on Plate XI, Sheet 1, and record section on Plate XV).

CONCLUSIONS.

Analysis of seismic results indicates the following geological features:-

(1) A major angular unconformity separates the known Mesozoic sequence(Great Artesian Basin) from a pre-Mesozoic group of stratified rocks,of unknown age or lithology, at least 16,000 feet thick.In the Westgate area south of Charleville, a second, deeper angularunconformity is present at a depth of about 12,000 feet. This unconformity is tentatively correlated with the angular unconformity at thebase of the Lower Carboniferous/Upper Devonian Drummond Seriesin the Springsure area, 200 miles to the north-east.

(2) The pre-Mesozoic sequence occurs asa series of large, truncated,asymmetrical structural basins or troughs, trending approximatelynorth-south. It is inferred that basement rocks (granites and/ormetamorphics) lie between the basins.

(3) The apparent absence of stratified rocks between the structural basins isindicative of deep erosion prior to deposition ofthe Mesozoic sedimentsof the Great Artesian Basin.

(4) Structural configuration of the Mesozoic strata above the deep structuralbasins is similar to that of the pre-Mesozoic but much less pronounced.This may be explained hy compaction of the pre-Mesnzoic or by slightstructural rejuvenation. Low-relief surface structure mapped on thesurficial lateritic zone appears to bear no relation to subsurfacestructure and probably represents topography at the time of lateritisation.However, steep dip of the "duricrust" on the eastern flank of Mt.Constance appears to overlie a fault of Late Tertiary or Recent age.

(5) Secondary folding is present within the presumably Palaeozoic structuralbasins. Further seismic work would be necessary to determine favourableprospects for a well location in order to test the petroleum possibilitiesof the area.

8

SPRIGG, R.C., 1958

WHITE HOUSE , F. W., 1954

REFERENCES.

Petroleum prospects of western parts of Great AustralianArtesian Basin. Bull. Amer. Ass. Petrol. Geol. 42,2465-2491.

The geology of the Queensland pcrtion of the GreatAustralian Artesian Basin, ARTESIAN WATER SUPPLIESIN QUEENSLAND, Appendix G. Dept. of the Co-ordinatorGeneral of Public Works, Queensland.

9

Date survey begunDate survey completedTotal number of working daysTotal number of shooting daysTotal number of moving daysNumber of shot-pointsAverage number of shot-points per dayNumber of recordsNumber of magnetic recordsNumber of holes drilledTotal footage drilledAverage hole depthAverage spread lengthAverage size of chargeAmount of explosivesAverage amount of explosives per holeElectric blasting caps

APPENDIX.

Statistics.

11

December 5, 1959July 9, 1960151(Average 10.8 hours per day)145 (1632 hours)6 (65.6 hours)8515.9174017531110135,645122 feet3480 feet (1740 - 1740)12.3 lb.21,517 lb.25 lb.2187

50

- -----'------ -f-- -----

1/ I

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30'20'

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---

2010

.... --20P _72P

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o.

C.1. =·020 sec. = 90'~DATUM =+600'

THARGOMINDAH AREAATP 72P-QUEENSLAND

STRUCTURE CONTOUR MAPON

IISLYTHESDALEII

0301 Shotpoint location 8 number.

@I) Terminal shotpoinfs of cross- sections constructed.

G-G' Composite cross-section used in this report

"",-,,;

II

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4

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ON

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20' 1------,

IIIII

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50'

20'

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I "'....."......,j;?""""""""""""....' __i"

THARGOMINDAH AREA

P 72P-QUEENSLANDAT R MAP

STRUCTURE CONTOU

ON 11

MESOZOICII BASE OF,+=·020sec.= 100_C.I. •

DATUM; +600

Bundtllo

LEGENO

. a number. nstructed.Shotpoint locahO~ f cr06S- sections coTerminal shotpomts ~ used in this reportComposite cross·sectlon=G-G'

MT. CONSTANCE",;,,<""

144°00'50'40'

40'

---- -,,,

, --

-_. ;20'10'

60-i'.72P

~.

\0'

30' --- 1l1/ I

'20' f----- I

Plat. III

SOP

r.'!~

C.1. = 100 sec. =800' ±DATUM =+600'

SCALE4 0 4 8MLS~'!!!liiiii;l!!!5OiZ!'!!!!!!!!!!!!!!!!!!!!!!!!5'......iiiiiiO!'

QUILPIE-CHARLEVILLE AREAATP 72P-QUEENSLAND

STRUCTURE CONTOUR MAPON

11 PRE- MESOZOIC PHANTOM 11

LEGENO

ShotpOInt location 8 number.

(@§) Terminal shot points of cross· sections constructed

A -A' through F -F' - Composite cross-sections used in this report

H -H' throuQh J -J - Composite record sections used mthis report

...~

f4 :°0 ;° ..' ; ,

•

!" •••• j i·,···· ..- - ~·~'OO

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::::----I---------t------I------I------I-----l---I----~~~~~r------+-------+------+---,+--~+L__I_----+_-----~30'

60PI72P---I

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8 I QUII~IA" ..1..·" .....• i'lE f •• ..1 11

I

~~~~'~'~~'0~!;':~~~~;;-r------I------I-----I------I------'r---I------1------t-------t-----~-____1------_+-----_J__+------~20'

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5'~~--~:f--------L-~,-----------;~----------t,;.-----------------;~-----------;~M'--------~-----------;,;;--------L---;;;---------tr-r--------------- --------------------------------144' 05' 20' 30' 40' 50' 145'00' 10' 20' 30' 40'

30'I-----~------I'--,~ki__::_::;~'!d

20'f----

27.00'f-----l+----------+-JL---------f-----------+----------1-----------i----------+-----------f-------+-+----------

'r~'~---l,0~'--------~T\---------,3T°'---'---------.:41o~'--------450~'-i------:::'14-;5.(0~0'--------~lfO'-i------~2To~'---------.:310'---'---------i40~'- ___l50~'-,~-----~14~6·r°l.C!0:...' --------T'o:...' ~o~'-__,~-----~26!iri" 05 146' 30'I W~

II

_-.J

Plale V

Sheet 1

AREA

Shothole LegendL = LoamC = ClaySi = SiltR = RockG = GravelS = SandSs = SandstoneSh = Shale

Datum =600' A.S.L.Ve =7000/sec.Vert. scale: as shownHor. sca le: °l;;;l;o;;;;;;iiiiiiI!""""''''liOi~~\~74~bi.'~'''''''''!iiiiiiil!!!!3~4IBO·

144°35'

TRAVERSE

Reflection Grading:GoodPoorQuestionable -- ---._-Survey by

Petty Geophysical Engineering Co.for

Phillips Petroleum Co. 8 Sunray Mid- Continent Oil Co.1959 - 60 Plate ID:

OF

30'

QUEENSLAND

SECTION

Location MapScale

I 2 3 4mls.; ; I ;

2.5

o!

--~----_.-//---............----+---

CROSS

SEISMIC REFLECTION SURVEY

OF THE

QUILPIE- THARGOMINDAH -CHARLEVILLE

144°20'

2G,°4d---+---------+-----------1---------f__-

210°35 -----j~--------+--------___jf__--------___l__-

.---------

4000'±

1700'::':

12000'+

16000'+

8000'+

20000'-r

Depth

+600'

Time

+500'

Elevation+700'

- . 500sec. =

- I·OOOsec. =

- 2· OOOsec. =

- I· 500sec. =

_ 3· OOOsec. =

- 2· 500sec. =

c:o

-Q)

Q)

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N

c:oU

R

c

I3231

I

c

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I30

c

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I29

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I27

5

R

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55-;;;:- -- -"5S?lP

I26

1804P

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94i!- - - - - - -;'3~p- -- - - --;3S?

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l?34F

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23

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22

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c

R

I

194"1F

21

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Surface

c

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1443

'::::::::'~'.. 1,\98P.................. l?2SP n~9 •

.......... ,'1S5P

--- ~~Ci>P-- --~9:::\P;;-------;gliF---';4"'iP - - -r;%f - - - - - i;~!,- - - - - -l;5i'F - - ---a9'2,<i>P 19~P - - - - - - - - - - - - - -1C2)I~F- - - -- -- - ~93P19'J9F 200SF lOI'1F 2018F 2.0t3F 19~IF ------1;82.p

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- - - - - 5815 /04F 559F 579F

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, I

AIN800

E.

FI F2

-

-4000'±

1700'!

8000'±

12000':t

Depth

Elevation

+ 700' t+ 600'

+ 500'

2·500sec. = 16000'± >-

2 ·OOOsec. =

Time

3·000sec. = 2000d:t '-

1·500sec. =

I·OOOsec. =

. 500 sec. =

Datum = 600' A.S.L.Ve =7000/sec.Vert. scale: as shownHo C I 0 1740' 3480'r. s a e: I;;;;l;;;;;;iiiiiI!~__~~\o;;,;;;ioiiii!~'liiiiiiil""""'!"!Il

Shothole LegendL =LoarrC =ClaySi = SiltR = RockG = GravelS = SandSs = SandstoneSh = Shale

144"35'

TRAVERSE A -AI

Shee t 2

30'

SECTION OF

2.5'

CROSS


OF THE

QUILPIE- THARGOMINDAH -CHARLEVILLE AREA

QUEENSLAND

144"2.0'

21i>°35'-----t--------j--------+---------l---

..._______f..--------I---~ ,.//~

-----t---

4000'±

12000'+

8000'+

Elevation

j+700'

+600'

+500'

Time Depth

- . 500sec. = 1700'±

- I·OOOsec. =

- 2· OOOsec. =

- I· 50 0 sec. =

_____ - - - - - 12.;?- -

----44"TP 44'lP4S9P

------------

1640

IN730E INBO.E_ ISB2.E. \S77.E. IS60.E_ IS69.E. ISB2.E. ISB6.E_ IS87°E

AIN87°E INB.E.I ..

31 32 33 34 35 36 37 39 40 41 42 43 44 45 46 47 48 49 50 51 53 54 55 56 57 58 59 60I I I I I I I I I I I I I I I I I I I I I I I I I I I I

Surface--- Ss 5""Ss

~Ss c R R ShR R R R.r-R R R~ R .J2. R ..§!. e'- ...£.. R Sh cR Ss Ss Ss c e c e

:::E c c C 55 Ss Ss ss Ss C cc I. c ss ec c I c I c c

It 11

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__~--- '''50F 1441P• }5!~P•• ' ., ••••• ISOIP

" ..... , ................

12000'± ...2 ·OOOsec. =

Elevation+ 700'

t+ 600'

+ 500'

Time Depth

. 500 sec. = 1700'! -Cl>Cl>.s:(J)

4000'±E

I·OOOsec. = ,... 0........

'0Cl>:::lc:

1·500sec. 8000'± ... c:= 0

u

2(j,"4cJ

2· 500sec. = 16000'± - - 2· 500sec. = 16000'+

Location MapScale

0 I 2 3 4mls.! . . . I

3·000 se_c. = 2000d± - ~ 3·000sec. = 20000'+

Reflection Grading:GoodPoorQuestionable -- ------Survey by


Phillips Petroleum Co. 81 Sunray Mid- Continent Oil Co.1959 - 60 P T7T

late ~

Sheet 1

8

IN63°E.. IN57°E.. IN63°E.. IN63°E... IN630 E.. IN64°E... IN64°E... IN65°E.. IN67°E.. I N64°E.. IN50oE.. IN81°E... IN84°E .. !N73 0 E.. IN73°E... IN83°E..

875 874 873 872 871 870 869 868 867 866 8?5 864 863 862 861 860Elevation I I I I I I I I I I I I I I I Elevation

+600'Surface ] + 600'..£ L C c -L -"- E

S L L c

+500.]

c - L L CSs Ss - Ss t C - Ss Ss Ss- - Ss Ss Ss Ss Ss :E - - -ss Sh - Ss -5h Si Sh - - Sh - I; Si Si S c

+500'Sh - - - - - Sh I - -- Si Si S, C C- - :::t c -- - ::::c - - SEISMIC REFLECTION SURVEY

OF THE

Time DepthN

Time Depth QUILPIE - THARGOMINDAH -CHARLEVILLE AREA

. 500 sec. = 1700'±-4G4?

503F - - -SOOP - - ---s'08'P---- - - 5007- -- - --'4q;P-- - ~tiP - - 4qiF- - - - - --;Ii?- - - -- - '4QS;"- - - - - - SO?? - ----- '500?- - - - --

5QW- - - ---SB4P

7:ff/ythesda/~o~;:;;'P------::7"0.6"'F---~70"'BF,-------::7"-04:'='F-----c:'70·':':.F:------::jO~- - --",71·8"'.,------=-,.,"',.----:7;";,0;';-.-----;;'0000••------:::'10·-=.----.,':;;.;0;::;••,-----0''00;'•..----'''0;;;;••'' -- - 10W - - -

...-Q)Q)

.l:Cl)

- .500 sec. = 1700':t QUEENSLAND

CROSS SECTION OF TRAVERSE 8-S1

144°30'

Datum = 600' A.S.L.Ve =7000/sec.Vert. scale: as shownH I 0 1740' 3480'or. sea e: l!!'!!!!Siiiiil!!!!!!!!!!!Iiiiiiil'I!!!!!!!liiiiiii!!!!!!!Iiiiiiiil'

Shothole Legend.L = LoomC = ClaySi = SiltG = GravelS = SandSh = ShaleSs = Sandstone

Reflection Grading:GoodPoor --Questionable --------

144°20'

8"8\110040'+---------------ir"

- 2·000Sec.=12,000'±

- 1·500 sec. = 8000':!:

- I· 000 sec, = 4000':!:

co

'UQ)

::lC

coU

1215?--- - ---06H'____ - --iil0?

1311;>

11C27P

= 8000':t-

= 4000' ±-

=12000': -

1·500sec.

I· OOOsec.

2· 000 sec.

Plate 3ZlI

2'500sec. =16000': - - 2·500sec.= 16,000'~Location Map

Scaleo I 2 3 4 mls., , . , ,

Survey byPetty Geophysical Engineering Co.

forPhillips Petroleum Co. SI Sunray Mid-Continent Oil Co,

1959-60

8 1 Shee t 2

I I

IN36°E.. IN52°Eb

848 847


OF THE

Elevation

]

+600'

+500'

sSs

c&G

!N50 W...

828II

Surface

c

c5

:;Os

\ N7°W..

829

Ss

!N8 0 Wb

830

...

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Ss

\N1BOW ..

831

Ss

~832

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833

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c.

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!N45 0 E.

843

S.

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844

...

845

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co.

IN38°E b

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849

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IN51 0 E..

850I

Ss

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851

s

\N55 0 E..

852

\N600E.

853

_L_

Ss

IN570 E"

854

IN75°E..

855

c

IN81°E>

856

LSSs

IN72°E.

857

G

....LC&-Ss

IN31 0 E..

858

....LSs

IN39GE_

859

c

...LS.

IN83°E..

860Elevation

AREA

8-8 1TRAVERSE

Datum = 600' A.S.L.Ve =7000/sec.Vert. scale: as shownHor. sca le: Dl!!'!!!!!!!!iiiiiil!!!!!!!!!!!!iiii

17;;;li!!!'o!!!,'§;;i;;;il!!!!!!!!!§;;3;iiil4.8D'

Shothole Legend.L = LoamC = ClaySi = SiltG = GravelS = SandSh = ShaleSs = Sandstone

Reflection Grading:GoodPoorQuestionable

OF144'30'

SECTIONQUEENSLAND

CROSS

QUILPIE - THARGOMINDAH -CHARLEVILLE

B2B\2"o40'-+-------------------l-!-

DepthTime

- .500 sec. = 1700':t

- I·OOOsec. = 4000':t

- 1·500 sec. = 8000':t

- 2·000sec.= 12,000'±

15';;~----- iS4~? -- ---1543?

112.'iP ---,"9P------i"it'8?-- --- -ii33P

1600P--- -- ~O'3?

_______ .!:'30"? 12.,,"-5?

\'lMOP 12.587" - - - - - - .

13DI~ - - - - - ~oa? - - - - - i3oo,,?

______________________ ±S2..?4517.---- 4S2.? 44&P MGP _

4Bc&? 47BP 4771" 4'7(01'

560P - - --S'l1P ""

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- !:-24?

--

4~n - -- -- - 4i'~r--- - - -~i:?--- -- - 4co7?

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-- -- - __ ._IQ04?

21'21?

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- - - ~ F s,gp-- - - -SE.8'P .- - --eG.5P - - 875P - - ---S,,"7'P" - - ----SoqpBiB? 'J~~:::F-----::'~O:5""F"----- -q"iqp - - ---qj3P qSqp- - - - - - - ---- -- -q48?--- -- - ii'4Qr- -- -- ---'5-""'- -= ?

__ • q5~? "I'Q5

---------?------iOI6?~iOI6?~iOl~";P---...-....-...q4P~I05S!"~IOir;?-~-'OliP~-.ollP --- _~I02.5P.............-.J02.4~ • --0- lO;l4f I044P~;;50~__~

- lOQ4P • " ' •••• '. '. - - - _ _ _ - - 11I'1? _ _ 'O'7'7P 10QlP

.. ,. -... - __ ~~~7__ _ _ _ lI'~n? -- --1l.1.~!___ _ t16-1?- - - - - - ii"fi""ir- - - - - - iisop- - -- - - -;-;;;:?, --- -- ii61?--- ---- "ii60? - - -1150"

' ••.••••.••...••. '.. 1'l]3P -- .!.C\~p_ 12.28P 12-'l;? - - -- - ~18?

·•·••. '32.dP ----_ 1ill? --'j2Q(;r--;;~f---"'" ~.~? 13471 ---ii'~p--- _

··is;5? .••...,: •..,: ••••.•.•.. __ 1413r -_ 1411P ii~;------i3cHR------i3~e,?-._ •• '. • 14C<o6P

........ _ ...... IS'03? • - •.•...•. ' ••• '. _'. ~48q? -- - __ ~~~?_

. -" 15~?-'- - -- - - j'SqZ? , 159'-?1f.2,4?- - - - - _ !.!'.&q?

'" - - - ~~r::::: - - _ ::5P I~q:w 16';~? - - - - - ';6;t? - - - - - ICD,?)?? 1~9iP ~84P 16"17P "Pre-Mesozoic 11

................. Pre-Me.~ . I 1"J4"Dr-- 17.q~p l;.S.7.f.,-.,-.,-.. -.. ,-,.'Y~~~~~.~.~.~.~.~~~\-.-'-~~.-~.~.ry~:f , .' ..... ....~~Z,..O.I.C.. ,', ---- '857P--- -- - - - - - - - - - iB - - - - - - - - le~6P _... -•... -""-.. , 5-8?.~·- - - -'8-S4?- - ----'S39i-·············

• • • • 18l2>!>F - - -- 8s81 se, IBt:.3P ., le-......... ----~o~· .\Q'S3P 'lC?02,? - - jq~'T? - - - _ . -. - - 'jqsi'?- - - - .. , ., .1960?. - - 192.SF

---- -- 20507 Iqaq? --~63P------200i'~------i;9SP-----~;a?·...:..:..::..--2002'?10'411- :::: ==-._ _ • .

-;'~14?

. - -;000' - - - - - - 4q6?- - - - - - SOl?

'0Q.)

:::Ic:..c:oU

-Q.)Q.)

.s:Cl)

Eo...-

Depth

= 8000':!:-

=12000':1: -

= 4000' ±-

= 1700':-·500sec.

Time

I· 500sec.

I·OOOsec.

2·000 sec.

2· 500sec. =16000'-:: - - 2·500sec.= 16,000':t Location MapScale

o I 2 3 4 mls.t • , • ,


forPhillips Petroleum Co. a Sunray Mid-Continent Oil Co.

1959-60Plate JZII

11 11Blyfhesdale """"79U---"Ta1F_______ ----S21P BOBF

842(' S38F

Surface

C

IS750E~ ISS50E~ IS790E.

299 298 297I I I

AREA

TRAVERSEOFSECTIONCROSS


OF THE

QUILPIE -THARGOMINDAH -CHARLEVILLE

QUEENSLAND

DepthTime

Sheet 1

- . 500 sec. = 1700'':!:

- +600'

Elevation- +900'

- +700'

- +800'

co

N

-Cl>Cl>

..c.en

c

Ss

c

Ssc

cc

cc.c

R

c

RR

cccc

s.

c

Ss

c.c

s.

c

Ss

c

Ss

c

Ss

cc

Ss..

Icc

IS36"E.IS690E.IS22I/20~IS221/20~~IS360E_IS560E.IS560E,IS5S0E.ISWE.IS7S0E.ISS50E,INSSOE.IN760E,IN670E.IN590E.INSOOE.IN630E,IN62oE.\N660E.INWE.IN790E,IS430E.IS690E288 287 286 285 284 283 282 281 280 279 278 277 276 275 274 273 272 271 270 269 268 267 266 265

I I I I I I I I I I I I I I I I I I I I , I I I

c

R

c

R

c

Ss

!S5S0E, IS700E. ISI30E.291 290 289

I I I

GSs

________ __ _- _ _ "Blyfhesdale"'81F --- - - -Tr9?--- - - - ~,;;-- ---:;;;F"" - - ~4P-- - ---1841-- --- -78S?-- --- - lBBP- - --- -7611- 11BP 1B~ - - ~B;;- lilSf 170? HOP 76"6 7rol? 717? 'EIS? l'-Sf ,.,.O? 'B4F 773P 7tD7P 71B;; - - - - - -7'&1 - - - - - -reS?- - - - - -lB9r- - --

\S740E.

292I

ccc

g,Ss

IS5S0E_ IS750E~ ISSIOE.

295 294 293I I I

ccc

R

1700':!: .-

Elevation

+800'

+700' [

+600' [

DenthTime

. 500sec. =

25'20'

Location MapScale

? I 2 3 4 rnls.

~~2ro.2:''-t----~---t_-------+-------_+

8000'! ~r----~v--__---+--S-ho_t_h-ole Legend:I L = Loam

:;: C = ClaySi = SiltG = GravelS =SandSh =ShaleSs =SandstoneR =Rock

Reflection Grading:GoodPoor --Questionable -------


forPhillips Petroleum Co. SI Sunray Mid-Continent Oil Co.

1959 - 60 Plate 3ZlII

16000'~

12000'~

- I·OOOsec. = 4000':!:144°'0'

- 1·500sec. =

- 2 ·500 sec. =

- 2· OOOsec. =

coU

20«.GP

--- ;;677- - _ _ IB2.1P---"----

------2022? - --

1945j 1954?

1594P

9751-- -- --";"a"'7

n~------iG89Pn02F

1624F

1"'lP11~~? -

- -1541?

11e.5?

9;;''(- - -- --;-/iJ-;-r---- -- 9lDl!- - ---- ;'15f- - - - - - -98-'".-- -- - - 9tt>SP""" - --r 9aS;;- - - ----g'B2P- - - - - - 989?

..-............ ...........---........................-------...........,......,....................------~----..........,......,----....--~-..........~-..-............------..........----..,.....,,......,----.........~.........................--...-------~- ............------.......,.............------..........----..,.....,,......,----......... ....................~.II2.IF ....----....--.,12SF "':::::::::::'22P ...-----.,...._.r......... ..............__... ~_............~ ....___"."~'o-;:....n·-,......,-.....-.r-~-........-.,:;;~O'J...? ..__... v--.....................~........... ...................~~..__...---..-. ,......, ...............................~ ........~.........._.._ ..__............._...r..,....., ............__ ~_~ ..,.....,.r'0~.:;;~?-.r-............-_-~-~-~;;_..-:;__p- -_-.....-~-_-__..._:.;;.:;.75:.;..? -,......,-.....-~-~-__- !f!.a~_ ' 1ll5P .........------~.;;;;-'Y._:'><'......................~..................... ~

1177?~7i&4? 1'.2.41P 1254P 1237P 1238? __ _ 114-IP-_______ -:------;3;;--- 12.13P -- '213F------72iti.j···· ._______ ~93?---- --';is,,? ----~7~==~~:.:=~75?-::::-i2BS;--- -1219P --~.;;----13?l""5'P----;:33P------133~--~~-- 12.64P ' '. _... 13;;------;;:i4F--- --l!a~F-__

• /I 131:"P__-----;'3'-i'76;;;G:----;;13;;;- - -134BF 1332F' 133'1P la31P 1335P ~52F 134f>F 1354f ... :..... ":': ..::~~?-.: __'.:.' '" .. . .. 1340? - - i3S4? - - - i3S-1? - - - _

"p e_MesoZOIC _- - - -- "l4o'G _ '47>' - - -'48·3·F·· :....:..:. ..::..:,........ 138"P - 14·'Opr _ J44SF _~~:!_-- --------___ I48QP .

- - - i498P- - 1499F - - - ~:Z5P - - 1521F IIp,1530P _ __ - ~~--~"7E.P 153;;---·· re-Mesozoic I

15gB? 'S~";?-- ---- 'i59w---- --7;0;'[- - -- 15G1? -- -- __ • ·1~-j2.P· " ". r-_--162BP --

8000':!: -

16000'~ L-

12000'± I-

I· 500sec. =

2·500sec. =

2·000sec. =

I' OOOsec. = 4000':!: ,....

Shee t 2

Datum = 600' A.S.L.Ve:: 7000/sec.Vert. scale: as shownHor. scale: o!!!'!!!!!!!!iO;;;;;;;;;l!!!!!!!!!__nil!!i!!!!o'!!'5ii;ii;;;I!!!!!!!!5_3~~Bo·

25'20'

Location MapScale

o , :l. 3 4 mls.; ;

IS'


OF THE

QUILPIE -THARGOMINDAH -CHARLEVILLE AREA

QUEENSLAND

CROSS SECTION OF TRAVERSE C-C I

4000'!144·'0'

1700'!

16000':!:

t-~2r".2:.--+-----'''----+-------~~-------+-

BOOO'! \. _ ~r-__-_--+--S-h-o-th-o...~e L~ge~d~oam'",-- ~ on C :: Clay

Si :: SiltG :: GravelS :: SandSh :: ShaleSs :: SandstoneR :: Rock

Reflection Grading:GoodPoor - -Questionable -------

Survey byPetty Geophysica I Engineering Co.

forPhillips Petroleum Co. Bc Sunray Mid-Continent Oil Co.

1959-60

12000':!:

Depth

- . 500 sec. ::

Time

- 2·500sec.::

- 2· OOOsec. ::

- I· 000 sec. ::

- I· 500 sec. ::

- +800'

- +600'

- +700'

Elevation- +900'

5.

SsSs

C

Cl

IS840 E.. IS80o E.

1129 130, i

5

c

Ss

128I

c

Ss

c

Ss

INB70E.

126 127I I Surface

R.

c.

ISBIOE.

125I

c

Ss

c.

Ss

c

SsR

INBgoE, ISB20E. ISB50E.

121 122 123 124I I I I

5

Ss

e

120I

R

c

ISB30E.

119I

c

Ss

118I

c

Sh

117I

c

!SB50E.

116I

ccSs

IB~?------ ;';91?

!NBBOE. !SBBOE,

113 114 115I I I

c

Ss

I~nr-- - - - - ';';2.'l.?

___________ --- - iicii'?--- -- --- -- -- - -jiBl?142.51 14~3? . 140iJ?

112I

6l;tiP-- - - - - 5GB?

Ss

II1I

Ss

-.§..c

110I

c

Ss

S

R

c

INB60E. ISB70E.

107 108 109I I I

Si>Sh

S

Sh

1904P

s

Si

98&? - - - - - 988P'" - - 98;;- - - --gew - - 9';;P - - &a9F"

-Si

L

'S;

c

Ss

11 11

704P '0'. B'lythesdole__''!J!Y!!!.~~d.P!e.-'~ __________ __ -- -- -- - -- -- - - - - - --- -- - - '138("-- -- -'1.<:>- - - - - --:;.O?--- - - - '1,j'; - - - - --7'2? - - -- - - ~,B.-=== -'3:- - - --:;;-0;;; - -- -- -<;""?

159? lSn 7B5-G----71"~F---~1B:""'F-- -7Bsr:- - - '1'g-,.----'81P '7a6""F,...---~1B·~..F~-----:"~-..'~F----1""-F----=,'3:;--F-- - -- - '74f '"70? ,Et,,!, 'E.4? .

-- - 970P--- ----;667992.P

...............---.......,,..'''""'"..___................,. ~..___ ~........... -----~----'''""'" .....................,...,,...................,.-------..,................----........-------.............-------~ ...........-~..,........-------~~-~---;;........-- 10';;;-~38P-~ ;'31? ~",...,............---.......,.---------~..--------~___~........ "....... ~II::;:OIP:....-.........,.-----~'~'07~F---~ ..................,.----",...,.............----~'O:;!'..8i::.,.P-~-,...-...........---....-....:.j'":::;10.~? ................. ..........._~.......... ..................._ ......... ........... ..........;.:110e3!:...p_-_-_-_..._':::-11I5F~ 11I1F'- ." II~? _ - - "ii~;?- _ ... "

"Pre-Mesozolc_ -- - -'- - -- .__ ------ 1260?

12.·S"'?"';-:· • " •• 122.6? _"-'- - -

. . . . . . . . .. . . ....:.: :.::...i3~;;- - - IS2CiJ'P - - -

• • • .. .. • • 13707....._ ...... . ....... ......... .''p M " -.

re- esozoic ................ .. r-__ -'iE.ii?- - - - - - ;;.>oP - _ .. ;".B'P' , ..• , :";4-?' - - - - - "'5'9? -- - - - 'U"?

173-;P---- --rr53?

S43°E. \S6goE.IN650E, IN650E_~ INB50E. IN610E~6 265 264 263 262 261 260

I I I I I I

+0

CoU

'0Q)

::::lC

Eo...-

Elevation

+800' I+700't

+600'

DepthTime

. 500sec. :: 1700'! ,.. ~Q)

£(f)

I· 500sec. :: 8000'! I-

\·OOOsec. :: 4000'! -

2·500sec. :: 16000': ....

2.000sec. :: 12000'± r-

Plate 3llII

D D1

IN39 0 E.

441 442I I

IN500 E.443 444

I I

IN3BOE.445 446

I I

SURVEYREFLECTION

OF THE

SEISMIC

Elevation

j+700'

+600'

+500'

c

'+Ss

cR C

c

R

c

Ss

c

INB5°E. IN90oE. INB3°E . IN70 0 E·457 458 459 460 461

I I Surface I I 'G ~

c

INBBOE. ~455 456

I IS

~

c

454I

R

c-=c

L

Sh

IN37 0 E. !N440 Eo IN760 E,450 451 452 453

I I I I

Ss

Si

c

R

L~Ss

c

IN45°E. IN4BoE.447 448 449

I I I

5

cc

L

Ssc

L

Ss

Si

c

L

S

c

Si

Ss

440I

LS,

Ss 55

C Sist

- c...=

IN3BOE.438 439

I ISurface

Elevation

+600' [

+500'

Time Depth Time Depth QUILPIE - THARGOMINDAH -CHARLE VILLE AREA

QUEENSLAND·500sec. : 1700'::

SISP - - - - - - -54D? ----541F !&44P

5:isF--- -- -5'17¥ - - -- - - 51S;- - - -5\~- - ~3'iP - - -S3iP--- --- 533? !i3~ - - 54;;- - - --r;2qr- ·500sec : 1700'2:

CROSS SECTION OF TRAVERSE D -D1

Plate ]X

Datum : 600' A.S.L.Ve:7000/sec.Vert. scale: as shownHor. sea le: 11;;;;;;i!!!!!!!!!5iiOiiiil!!!!l!!!741i, o.·00I!!!!!!!IiiOiiiil!!!!::!>!!!!!If80'

Shothole LegendL : LoamC : ClaySi : SiltSist: SiltstoneG : GravelS : SandSh: SholeR : RockSs: Sandstone

Reflection Grading:GoodPoorQuestionable -- ------Survey by


Phillips Petroleum Co. Bc Sunray Mid -Continent Oil Co.1959- 60

+

144°20'

Location MapScale

o I 2. ::!> 4ml...; .

144°15'

26°35'_-+ -+ -1__

4000'±

8000':!:

16000':!:

12000':t

- 2· 500sec. :

- I· 500sec. :

- I· 000 sec :

- 2·000sec.:

----127.3F1300P

1454P

1~4GoP

131lSP

-~1~--

142.2.P

1326F

14,bP __---1437 f

2.IIO?

1I5i?- _ _ _ _ _ _ 1I1~~ __ -- --ri'lq;- - - --0,i'i' -__• • 1I1QP 12.~6F -----

11I'ro-----__ ~--·~----_;;0i;;;;_----------.::12.~ 113~S,? _"Hi7G 130$F _ _ _ "i2.87?- - - - - - tlB2?- - - - - - ii8'&P - - 1300;'" - - - - - iS04'r

1330F __ - ~~~ __ ---

-- --!!9:!:---_-..!!~lP-----

--

q2.iP------qU? ClClBP q33?------q25P

'l8~--~liF- ---'OO1P------iOior----- -i01liJ? _--'""""'"iOI~------n&2P--~ii?------ iOi2?------iOIQ?----- -iCo,,"p IOO2.~ -- ~liP------iOl!S?1l)40P ".

11 l~sq? •••••••••••••••••• " ••• u IJpre - Mesozoic 11

Pre.:M~$.QlSl.ic. :~e2P ' ..••. ' . ••...... " ..•. " ....•. " ..•..•..•............ " ',',e'2'," .. .:...:..:.:..:.:..:~ ..:,p' :,;'-1':' :..:.:.:.::": :.: ~~~;':''':::'': :.:.::;;~:: .~ '.:.:..:~,ip:-''':'':'".-':.::' ~:.?---ni'"5?---- ~;-:..:.:~." " ".. ? ---~~?-=----,804-P -- "

. i814? iq25P" • • • • • • • • .. • • .. • • .. ' • • • • • _ ~~ _ - - la24P 11Q3P - ~07P - - - - -181~?, IB'lqp.................. , --- ta~--~56P

1885P IIq~6P _ - - - - 1Bq1?- IQO'iF- - - - - - '9ill18?

IQS4P --'::'_ _ Iq;.P ---ioior-- _

- -' - . 20W - --_.J-0.!.5.!.._ - 2OT6~

- - - - 21nr:- -

8000'± f-

4000'± f-

16000':: -

12000'+

I· 500sec. :

I·OOOsec. :

2·500sec. :

2·000sec. :

3480'!

AREA

Sheet 1

Datum: 6001

A.S.L.Ve =70 OO/sec.Vert. scale: as shownHor. scale: L 1740'= ;;;;;J

Shothole LegendL : LoamC : ClaySi : SiltG : GravelS : SandSh: ShaleSs : SandstoneDur: Sandstone

Reflection Grading:GoodPoor --Questionable -------Survey by


Ph illips Petroleum Co. a Sunray Mid - Continent Oil Co1959- 60 Plate X

OF TRAVERSE E - El

30'

SECTION

QUEENSLAND


OF THE

Location MapScale

°l!!1!!!!!!!I;!..;iiI!T!!!!!!!3!;;,..;;4t mls.

25'

CROSS


0'

/"","03

s'

j - -

....SIS

0'

2·500sec.: 16000'+

2·000sec: 12000'+

"OOOsec : 40001±

I· 500 sec. = 80001±

3 ·OOOsec.: 20000'+

+ 900'

+8001

+ 700'

Time Depth

. 500 sec. : 17001±

Elevation+1000'

c:o

c:o

U

N

-Q)Q)

.r=(J)

c

Ss

11.;:;;'"--00

c

IG~--~79P---

c

Ss

3~------U~------~~------

c

Ss

la5i'P - - --;:,;;:-- - -;-;;;:;- - -183&P

c

Ss

1t..-4--V-----I"Ise:F - - -'ISOP

'l03:3?

593I

c

Ss

c

Ss?

IS8S0 E. IN78oE.591 592

I I

c

Ss?

- 79~? - - - - - 2000; -

----209(,P

c

Ss

14"J~--~"9P

c

Ss

c

IN840 E_ IS890 E. IS820 E_533 534 590

I , I

Ss

532I

1115V- - - - - - iie~?- - - - - - iTs.!!:.. _ 12.43P12CD1P 12.2.7P - -

12~? - - - - - ii:; - - -;;;8P - - ti&;P - - ~~5P J2~ - - --;;81P

c

531I

2040P - - Z045P

I"SOP

c

530I

c

Ss

529I

c

L

Ss

12.i5P - - --;i35P

1'3;'; - - - - - iiS5?

528I

c

Ss

c

Ss

nli? - - - - - - nS7P

c

Ss

JSOW - - - - - - iSl4-?

1!5S6.P - - - - - ii:o!t?

19m - - 194"iP -

1'1.1';;- - -""IiiiP - - -'2.'!oCDP

c

Ss?

IN870 E. IN83°E. IN88°E.589 525 526 527

I I I I

I043P loiOP'-----i5I1? IO~30P

_ .. ~,o"it::'; :-..:::;-;;,=...............~ ~ '011'~-::.......O·E>SP --...-..~--......------_........_----.......--....- ...-...- ....-~~IO~~OCQ6P ~I05;P"""::::;::::'I059P-;::":-:'-::'= iO&87~1I3G:'P- - -- - - ii4;"r- - - -- - ii53?

11.~ - "'I'i.'l.SP

t34iF' - -';r..O'P - - -';"3P

c

588I

______ !.~14P

c

SS?

145;;- - -.A.COI6F

-i5"J2?----- - - -_• t!593P llOO'!!t

"Slyfhesdale" .5S"':,?-------509-r-P- ,_ __ __ __ _ '55D?

• "-'4P C02.2.F ~2.7? 1Q31P E:>2.7P EJ2.5? GU&P C010P 6'lOP - - i~i?- - - -- - ;40F- ---- - G4-:;~- -- - - - 61.iP--~i'8P ---- - ~2i?- - - - - - - -- - -- - -i2~ - -~2BP- -- - - -7:2~!--- - - - 6'1W- - -~23P---

,,;;;- - - --=j,gp '207-- - -- - __ _ _ 68-;;;:-- - ~~"iP- - ----6'6S? G8"iF-- ~S;;;---~s4F---~a;p_---"Jii>;:;-" - - ~",2.P- - - - - - '71? . i34F 74'1.? "J34F' 13GP 801.1

_ --- - - - --75t9P--79;;- - - 00B40F' 840P B~8P

IN8S 0 E.581 587

I I

--918P ---

2014P

~~-_.---------- 11 ---;-02'iP-,.;-.... " " .•.... ?~5?? ...•.•• Z069V 'OllP Pre-Mesozoic...................................... ...... . ........ .

2.2."i'o"f-----22~~? :~~5!.~.~.-..~~.. ~:1~~....... I1

23iiP 231" '" '" " . .t::::e.-MeSOZOiC"................. ~-:':'"' .."

1832.1---_._----

IN82 0 E. IN900 E.583 582

I I584

I

c

Ss

c

Ss

c

S5Ss

c

L

Ss

IS890 E..,520

I

\\

Surface

c

COIM - - ~I:W- - - ~17.P

GsT - - -/ii90P1~ _

____________ - - - - - - - -:;011 801? 7<D4P "7"9P - 7!:JiP-791?~"le5",,~'l8"3?~B·~p~81~~'Z.e.F__"""" """"_V';:;':;__

Ss

iI 11

410flIY_th_esd~:-:-v----"'''6;F - - "4s;;;;- - - """"'4..", - -""""'4"'P- - ---- 4.i<:"?- --;;;Sl?····· "'--"""4sip--

Elevation

+ 900l

t+ 800'

+700'

Time Depth

. 500sec. : 17001 :!:

I· 500sec. : 8000':t

I, OOOsec, : 4000':t

3·000sec. : 200001::t

2·500sec. : 160001+

2·000sec. : 12000':t

AREA

Sheet 2

OF TRAVERSE E - ElSECTION

QUEENSLAND


OF THE

CROSS

QUILPIE - THARGOMIN DAH - CHARLE VILL E

4000'±

Depth

1700'±

:;

:;

Time

. 500sec.

I·OOOsec

+ 900'

+800'

+ 700'

Elevation+ 1000'

ccc

Ss

54'S?- - - - - - S52P

cc

cc

Ss

c

Ss

cc

Ss

c

~7S? G~4P - - ~89P

.,,,4'P--75 4P

Ss

c

SsSs

c

Ss

,2.a.e- __--;o'iP - - - - - 66!'j?

_-----15SP6~ 'TBtP

c

INSOW. IN7o w. !N40 E. IN20 W. INS40 E. !N730 E. !N840 E. IN600 E_ INSOOE. IN400 E.\N430 E_IN420 E_ IN370 E. ~ IN400 E. IN760 E. E'600 601 602 603 604 605 606 607 625 626 627 628 6 9 630 631 633 633

I J J 1 J I J I I ISurface I = Ss sss

c

I

Ss

c

L

ss

c

L

ss

~ INIOOW.544 545 546

I I I

c

L

ss

SU?'- - - - - - S20P

543I

L

~

c

L

DuI'

c

874P - - -a,,~p8~,F

LOUP

c

IN260 E.~599 541 542

I I I

L

ssc

c

L

Ss

IN'90

E,597 598

I I

L

Ss

c:

L

~

c:c

B4tC?-- -- -S42.P

c

.J:....Ss

cc

Ss

c

L

:E:

"81y thesdale 11

-----7. -------------------- -- --- -- -4Ifr?--- ---:wo;- -- ~5P------"i'03?________ ---:4i,-.------;;:4"'SF 4&* - - -;;~ - 435P 4303P 4'300P 47.5?

"8 '/ - - - 54aP" - - 525P- - SosPIyfhesdale &2&P ..30G ....oSP--S';O'--- .......B1P----=t;4p- 62.~--~23P- -G'2"""P"...------:CD24F ,,~:;;z.~-----="~'3'ZF----:SIF ==== ~5'.:::OG:::.....----..3-5.-------,.,E.3.'1F 631P' 62"P 615? COl~ -------OZS3?- ---- - ~4~ - - 62SP

G~4'F"--~~---f,8~P ,,';:--. ----.:rosp co,..,p ~CD~P ."71~ - - -'18P 'ID

7"'?;P - - """"1Q,1.P

Q)Q)

~(f)4000'±

Elevation

+ 900't

+ 800'

+700'

Depth

1700'±

:;

:;

Time

·500sec.

'·OOOsec.

34BO'!iOiiiiiJ

Plate X

Shothole LegendL = LoamC :; ClaySi :; SiltG :; GravelS :; SandSh :; ShaleSs - SandstoneDur= Sandstone

Datum = 600' A.S.L.Ve:; 7000/sec.Vert. scale: as shownHor. scale: L 1740'

!""""""! !iOiiiiiJ

Reflection Grading:GoodPoorQuestionable -------Survey by


Phillips Petroleum Co. Se Sunray Mid - Continent Oil Co1959-60

30'

Location MapScale

I 2 3 4mls_I ! , !oI

145'20'

o'

/""<003

315'

_1 - -

-51""

o'

2",'

2(0'4

2",'3

12000'+

8000'+

16000'+

20000'+

2·000sec =

2·500sec. :;

1·500sec. :;

3 ·OOOsec. :;

'J.3?g? __ -

. "---

rJ64P

19~1?

18<06'1'

11881=" ••.' .,~, • 11

'''~~~~?:: ;::.:;: :: :: ::' Pre - Mesozolc-- --'lOIQ? '__ ::. ::: .... -

'20.76P _- _-

21001="_ - :: :: :: - -, 21~4F __ :::::: -:..- -

__ - ....- 22.59F 1'2.0ap·.---:::= --

1'294? _ - - '1~~---___ 13~__ --

2313P ~I=" __--'l~:~

217'lP ---zw~---- .25lCgp _ - - - - ~~I"..F. _.,

24,IP

----

304CQ?

-~-----~~f-----~~p-----~U?----~09/O?

2~09? __ ------

.... ' ... ........-----__ --"28&2? - - - - - 2B'B?

- --"2B;;?

- - - - - ii01?

~1ii'P - - -atiW - - --'i'liT - - -aoBi'P 3.gu;- - - --"3\BiP - - 3ilCOP

:!oDBS?

_-- -"'ilcc~;- - - - - - iia9?1lasp

- - - - - - - i2i5f - - - - - i240?17.B'2?

11005P- - ~94P

20S"lP

-'-IS40P -18'T3P

- ---;SB":iP - - - - i5~"'"ap - - - - - i'57')'"

-20~

IISg;--- li&lP

......'"

-~w---

- - -11"'1»'- - -IIBS?IISIF

23,~2P

'2419P- -':::'IP-- ••• - ••• 2.S·24P

'. , ".

1~G'e"P - - ~7-;P- - - -no,p

'2rn - - --;~OP

-le;';P - -183~P

.~~::e. -Mesozoic 11" " - :-: ":' :- --= ~~~?... ::---

"0Q)

::Jc:..c:oU

Eo.........

8000'+

20000'±

16000'+

12000'±

:;

:;

:;

:;I· 500sec.

3'000sec,

2 ·500sec.

2,OOOsec.

IS290 E.. IS45

0 E. IS76 0 E. IS75 0 E.. IS77 0 E. IS67 0 E.. IS61 0 E.808 807 806 805 804 726 727

I I I I I I I

Sheet 1

Elevation

j+ 1000'

+900'

+800'

5

L

Ss

sS

Ss

c

Ss

c

S

L5

c

IS77 0 E.. IS57 0 E.. IS52 0 E.IS65 0 E.IS600 E.. IS450E.. Is 13°E..

771 732 733 734 772 773 774I I I I I I I

_L_S

-c-

INI8 0 E.. IN290E ..

768 769I I

Ss

L

..L

c

5

cc

L

c

S

c

S55Ss

!S25 0 E.. IS28 0 E. IS43 0 E.. IS580E..

729 730 731 762I I I I

5

Ss

L

-"-c-;;;-

~ IS5?OE.. IS310

E799 798

I I

c

800I

:'>5Ss

c

803I

Ss

IS51 0 E..728

I

SsSsSsSs

cc

L

55

L

c

Ss

c

Ss

IS63 0 E.725

I

c

FIS31 0 E.

724ISurface

Ss

Elevation

+1000' [

+900'

+800'

AREA

Datum = 600' A.S.L.Ve =7000'/sec.Vert. scale: as shown

o' 1140' 3480'Hor. sea le: 1!!!!!!!'§iiiiiiiO~5iiiiO;;;io! ~iiiiiii~'!5;;;;;;;oJiiiiiiiI

Shothole Legend:L = LoamC = ClayR = RockG = GravelS = SandSh = ShaleSs = Sandstone




1959 - 60 Plate XI

OFQUEENSLAND

TRAVERSE F -F'

3 4. rnls.i I

Map

SECTION


OF THE

10

LocationScale

o , 2I I !

CROSS


os'

-t-

14"·00'

~~h._...... /r----,---_ __.

"-../' '14"-

2Go40'--l-----------I------------t-----------r-------

2CO03S'~'-I------------1----------t----------t---

- 2·500sec. = 16000'+

- 3·000sec. = 20000'~

- 2·000sec. = 12000'±

- I·OOOsec. = 4000'1

- 1·500sec. = 8000'1

Time Depth

- . 500sec. = 1700' ±

coU

co

'UQ)

:::JC

N

-Q)

Q)

.cCl)

----

1'2.21P----------

2141?---ijl;'?---:z.095?

--146&;--1493P

2.0b'ZP---_._--

-------26 13? l.:o'"&8?

__ ~':.:.?- _-- - - ii~y-

___ ---i330? -- --;'302.?

ISfO'?>?

24;'1?

244&?- - _ _ _ _ 15.?>fi>?---

."leG?

50~ - - --;-17..e....- _

5501- - - - - - 549P - - -SlOP 542P 54-5P 542? &39?

f04OP--~P

2324?

.......... .... ........

.... .... ....

- ---- ';9ssf"- ---__ 1973?

-- :::::::: ::::- _ "~~OP- _ _ 2J~7? ---.::::. _ - __ 2TZ2.P

----- --_--_ 2,2.09:>-- -- ..'2'20

1? - - -::: ............ .a..23fi>P

....----:::::

11 11

... /.,0? E}(y!~,,~;.P2Le__ -"2s:;,------'''ii·········· .-.- ~ -:-:-: ~ 2827- --- - -i"88?······ '319P-- - -3>5"- __ _ __ _ __ _ _ 'Slythesdale 11

34€1? 340? 3042"- - - -- - BSi? - - - --

408?- - - - - - 414P - - - - - - 4ifo?

-----..... '$1..... ~~:: _ _ 1&127

- - :: : ~~ __ l~g8P

-- -- :::::- ::::::::: -- __ 1155P n7:l.F __ '2s;.? :::: ':;. - =: ~2!1 11 • /I

'724P - - - 1793P _ - - - - - - - - -- 'i";5~?- - -_.!l8_5P_ 1'70'- - - - -'77" Pre -Mesozolc-- -- -- - - -- ISIB? IB27P ~~~ -_- _ -'7~7-F - --'7i6P- - . ~

17B4P - -- -- - == =.=:=== -=== == ~i6~ (BGO? 18E.'l? 1877? _ ~~!' - - - ==!= =. ==: : I=~: •.••.• _ ---;'8';;- '" -'.' . isi9? , ..IB"l7P \856P ISS4P - - -oem == == =-= ='= ===============::==:.=:: - 18';;7- - - - - - '8~1O? 'SliP - - - i&S6!- - 1677p- - - - i8eo?

1901P ISglC±? 190""?

.. '. '.

188F--- - - - i;Q4?

2744P

--------3ICDS?

-----\100? ........... - ................ ~"9?

17tG4? __ -- - -'-------18501 - Ie.;;?1907'7

- - --.:...':'" _ .2,9}'2.?

241O?

11 11B/yfhesda/e , , , ., .. , ie3'- - - - - 7:,,;,--- -- -1567- --- - -i"s.ry- - ---- i"si'F - - - - - - i4':i' '" " 'i':,,',' 25"';

322?--- ---311-;------- -- - --'"ii2'?"'Depth

= 1700't r-

Time

. 500sec.

I·OOOsec. = 4000'± f--•

2·000sec. = 12000'+ t-

I· 500 sec. = 8000' ± f-

3· OOOsec = 20000'± "-

2· 500sec = (6000':±: t-

Shee I 2

Elevation

j+1000'

+900'

+800'

c5

c

c

Ss

744 745I ISurface5

c

c

Ss

797I

c

s

Ss

796I

c.

c

L

795I

c

55

5

794I

5

c

c

793I

s

792I

cs-E::

c

L

55c

Ss.

5

Ss5

L

cc

c

5

c

IS860

E> IS86 0 E_ IS860 E_\S86 0 E.. \S86 0 E> IS86 0 E>

788 789 790 741 742 743 791I I I I I I I

5

c

L

sc

L

IN290

E IN470

E> IN310

E>

785 786 787I I I

c

L

SSc

L

c

L

Ss

c

L

c

LL

5

c

\S82 0 E _ IS670 E.. \S440 E IS540 E> \S66 0 E> jS84 0 E> IN61 0 E.

781 782 783 738 739 740 784I I I I I I I

5

c

780I

c

L

s

Ss

c

L

Ss

sC

5

cc

L

5

55

Ss

-c-

Ss

~

Ss-c

IS68 0 E. IS67 0 E.. IS82 0 E> IS790

E> IS770

E> IS520

E.. IS840E_

776 735 736 737 777 778 779I I I I I I I

S

775I

5

Ss

_L_

IS45 0 E> Is 13°E_

774I

s

773IElevation

+1000' [

+900'

+800'

AREA

Datum = 600' A.S.L.Ve =7000'/sec.Vert. scale: as shown

o' 1740' 3480'Hor. scale: ~!!!!""liiiiiiiOl~!IiOiOiZ!""'!!"!I__l!!"!!!!!'5iiiiiiil'

Shothole Legend:L = LoamC = ClayR = RockG = GravelS = SandSh = ShaleSs = Sandstone

Reflection Grading:GoodPoor --Questionable -- - -- ---

Survey byPetty Geophysical Engineering Co,


1959 - 60 Plate XI

OF

QUEENSLAND

TRAVERSE F-F'

1410°\5'

.3 4. rnls.I !

Map

SECTION


OF THE

10

LocationScale

o I 2-I ! I

CROSS


os'1410°00'

~~~_~h "4"

26°40'+---------+-----------+---------+--------

2(O°35'=---t---------+-----------+---------+----

- 2·500sec. = 16000'1

- I·OOOsec. = 4000'1

Time Depth

- . 500 sec. = 1700' ±

- 2·000sec. = 12000'±

- 3·000sec. = 20000':t

- I· 500sec. = 8000'±'

20.~O? - ---

:U24? _--------- _._'--

-------- IS9&f

2 185?

18M? -- -- -i&~?--- - - i89'2.?

44.2,? _

4B!?__ - - 464P - ~5"P 41~ - _ - - 434P

_------------52~? S~4·P 411?

sr:-iP- - - - - - 5SGo!' 538P" 544F S4COP 5621-- - -- - S88P6'2.:r?- - - - - - ~2iP - - - - - - 62.2F- - - - - - E:'2J?- - - - - - 'i,..,?

11~'P :!.~.!l--- ----2'~~ ___.22.IG!,

1l'2~---1J37P

_______ !1.45

?11.~8? - - !!.3~? - __

• 12.81(' 1271::>?Il79r:11.7SF

95~ - ---;;;,,"'8"'",----::'9G~ - -",ssP

----~w-----__ -_~~

- _ _ _ _ 10o"i?- - - lO"33F-- - - ~31P- - - - W4B?10GB? - ~.. - - - 2098?- __

212B?

22ii"P""'-~23'lP

l'2.'2.IP112S?- - - - iiS:T'? - - - - iTs.;p- - -1154P

l.3S;--- -- - ----~------ ;23"';;--- -i2.I~~

ISBOP

1649P ~~:...-- -:-:== - - --mB'i'P - - ~ ..;;"p- - - - - - ';;9-:;?- - - - - - _lo~OF ~ __ llOlIP ICD2.lP1704P -

• _-t74,;4?" ::.:,;..:.. ~ ..- - '''7ap"Pre -Mesozoic fI _ .•.....••.•••..••.•...•• " ••••.•..••••••• , •.••• 'I7S'2.?-~·'7 ;-.'7~.;';''';;;:'7.-:-:-: """"":-:;732P' ••• , •• _--

.. .. ..... - ..... ".... - .. - - - "'1'81;- - -n98P - - - - i7~;'( .-. " . " .. -ISW- - - IB'2'3P '8~7?

490' ---,-

513P- -- -- - 5ii?, --- -5i~-- - - 4e.2F 48&F- - -- 4S;?- -- - - - 495?

____________________________ ~'35!--- -SB':tF

CP3S? ~:l2.? 6'19? 103,P ~40P

11 1111 B/ythesdole

__ Blythesdole 11 34!L " 311"- - - - 'o"P-- - - '",,1- - - - .o..? · ····· .. ···· .. · .. ········· i'''8?-- -:r..;:?----;:..,?

342?- - --- - 3Si'? - - - - - - 1'~1? ~4-"r 3043,? MtP 341? 344? •••.••..• " •..•.••.•.•••••••... °3BO?- -- ---"'i1S?- -- -- -a1ii?- ---- -"3","9P - 3<D~ - ----;-,i'P - - -- 3"",j;-- - - ;;9?- - - - - -35:;:;>- -- - - - aS3?- - - - - - 35i?- - - - - - aSI? - - - - -- 339? 332? .

'0Q.l::Jc:c:oU

-Q.lQ.l

£(f)

Eo...--

Time Depth

. 500 sec. = 1700':t ~

2· OOOsec. = 12000'+ ~

I· 000 sec. = 4000' ± ~

I· 500 sec. = 8000' ± ~

3·000sec = 20000'± -

2· 500sec = 16000'±-

G G1

Datum: 600' A.S.L.Ve: 7000'/sec.Vert. scale: as shownHor. scale: 0l!!!'!!!!!!&iiiiii!!!!!!!!!!!lii;;;;;;;'74I!!!!'d!!!!!!!!lii;iiii!!!!!!!!!!!lii;;;;;;;IM,BO

Shothole Legend:L : LoamC : ClaySi : SiltR : RockS : SandSh : ShaleSs : SandstoneOur: Duricrust



forPhillips Petroleum Co. a Sunray Mid-Continent Oil Co

1959-60

-f-

SECTION OF TRAVERSE G-G 1

143°05'

Location MapScale

'? t 1 i rnls.

CROSS

143·00'

:w -~

424


OF THE

QUILPIE - THARGOMI NDAH - CHARLEVILLE AREA

QUEENSLAND

26°15

28°20

. 500sec.. : 1700' ±

I·OOOsec.. : 4000' +

I· 500 sec.. = 8000' +

Elevation

J+ 500'

+400'

+300'C&SS

5&5"

Surface

,N860W/424

I

\5680

E.. !S840E... jS860E..

421 422 423I I !

415I

414I

413I

GI4P---~2~ - -~2.w-- - &:z.qp- - - ~a4P------624?------62.2P------------- ---------- - -- ------ - ----- -------- 623i'

"Blythesdale"a;ap- - - 8,*~ - - -qO=OF----=qOq=G------;'q'O="G------;;;qO=SG----=:qo=.. ----::cqo;;r- - - - - - - - - - - - - - - - - - - - - - -----qosp

"Base of Mesozoic"I03{;P - - --;05::::-IF--~,0..7,::JG----::::IO"·";"::lG----=,O"=7G-------,.".,0,,~"G,...------,.,.IO_qF- - -;;)i:6P - - -- -- -- - - - - -- - -- - - - - - - - - - - - - - - - -- - - - - - -- - - - - iO'~?

15670E... 15720E...

410 411 412I I I

L

Ss S

c s c s; s sSs - - c CSh R Ss R C

Ss ssc I c

..L

4881" - - - - - - 4737

409I

""Btxthe.§!!!!~e_771? - - 751P

• • 11

"Base of Mesozolcq~-- Q01P

cc

c

c

IN860E... 15720 E.. 15630E_

416 406 407 408I I I I

c

c

\N820

E...

418 417I I

Unreliable data

cc

R

Surface ----.-----;;o:::::up---"'DU;;.-r--.---~--------_rs s. s. S

R

\N790

E..

420 4191 I

+200'

+300'

+400'

Elevation

+500'

·500 sec.: 1700':!:

1·000 sec.: 4000't

1·500 sec.: 8000':!:

Plate XlI

Time Depth

.500 sec. =1700'±

1·000 sec = 4000'±

I .500 sec. =8000·:t

2·000see. =12000'+

ifllJ}»1JJTII-r~t·iHlHiliilt:1-liiI...u-&.I • .u -

II/JJ;m~S1(r.~rrf'1f:~-'), ) .. , . if'" ,)7"~1, f l" -; ..} I

y-\o~ ,IIIJU I, _ t. t J...... 8'"I N :J,J""~..t

~". }')'~r .f " -, ~

~If ~))1 ~ .! r ~

,I I

I

}} }} ,rr :. ~ A )J I 1 I"

" U la.- 'lII ~ -...~

I l I ( .. I _

: . ,l I !t1)l ~.' I

- < I II .

I I > II I

II

.

II I

AREA

Time Depth. 500 sec. =1700'+

I·OOOsec. : 4000''t

1·500 sec. : SOOO':!:

2·000 sec. =12000'+

---.. I' \" })

I I

'}1- - - \,_

I ... /I i'!_ IHH+~

J

, I

I) 1 A I 1) It ~_-~t+-H-f+f-H)tH H}'!f-f~:Hl

....-H-l-++

~ ») I) }'i -~.++tt+t~ f\I

I~ - I ". - \ I

ill . ! i. i.[ . ..: .... - . .. ... t " I- tit I I ,:. ~r i (r, I~, t _~ ~ I 14w ~

r

- I I

Time Depth

·500 sec: 1700'!

1·OOOsec. : 4000' ±

1·500sec. = 8000'+

2·000sec =12000'.1

2·500sec. =16000'±

Time Depth

.500 sec. =1700'±

I-OOOsec.= 4000'+

1·500 see. =8000'±

2·000sec. =12000':t

2·500sec. =IIOOO'±

davince tools generated shot-points were spaced at intervals of 1740 feet alongthe line and geophone...

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