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1

REPORT ON ADDITIONAL SOIL SAMPLING IN THE VICINITY OF THE

MIRON COPPER-SILVER-GOLD OCCURRENCE TANNAHILL TOWNSHIP,

LARDER LAKE MINING DIVISION NORTHERN ONTARIO

For:

Brandy Brooks Mines Limited

8901 Reily Drive

Mount Brydges, Ontario

BY: Robert J. Dillman

Arjadee Prospecting

May 17, 2019

2

INDEX page

Summary 3

Location, Access 3

Claim Ownership and Logistics 3

Land Status and Topography 7

Geology 7

History of Exploration 9

Survey Dates and Personnel 10

Survey Logistics 10

Results of Soil Sampling 11

Discussion of Results 18

Conclusions and Recommendations 18

Certificate of Author 19

References 20

Figure 1. Property Location Map 4

Figure 2. Property Location Map 5

Figure 3. Claim Map – Survey Location Map 6

Figure 4. Geology Map: Tannahill Property 8

Table 1. Lower Quartile Derived from the Assays of Soil Samples

collected in 2017 and 2018 from the Miron Showing 12

Table 2. Summary of Rock Samples from the Miron Showing (2017) 12

Table 3. Response Ratios for Soil Samples from the Miron Showing 13

APPENDIX

Soil Sample Location Map scale 1: 2500

Soil Survey Map: Copper scale 1 : 2500

Soil Survey Map: Silver scale 1 : 2500

Soil Survey Map: Gold scale 1 : 2500

Soil Survey Map: Arsenic scale 1 : 2500

Soil Survey Map: Cobalt scale 1 : 2500

Soil Survey Map: Nickel scale 1 :2500

Soil Survey Map: Vanadium scale 1 :2500

Soil Survey Map: Zinc scale 1 : 2500

Soil Survey Map: Manganese scale 1: 2500

Soil Survey Map: Lead scale 1 : 2500

Soil Survey Map: Total Count Au + Ag + Cu + Pb + Zn Scale 1 : 2500

Soil Survey – Geophysical Compilation Map 2017 - 2018 scale 1 : 2500

Assay Certificates

3

Summary

On August 20, 2018 Brandy Brook Mines Limited collected additional soil samples in the vicinity

to the Miron Cu-Ag-Au Occurrence in Tannahill Twp., Ontario. A total of 15 soil samples (G-80

to G-95 inclusive) were collected by James Chard and Robert Dillman. The samples were

analyzed for a 54 elements by EDTA Cyanide Leach, ICP-MS finish by AGAT Laboratories. Results

were low for most samples. One sample (G-87) showed elevated concentrations of copper,

silver and manganese.

Location, Access

The Miron Cu-Ag-Au Occurrence is located in Tannahill Township in the Harker-Holloway

area of the Larder Lake Mining Division in Ontario (Figure 1). The mineral occurrence is located

in mining claim 529540 on the boundary between cells 32D05J363 and 32D05J364 at UTM

coordinates: Zone 17, 593854mE, 5363948mN (Figure 2).

The Miron Cu-Ag-Au Occurrence accessible via trails and logging roads connecting with

Highway 672. The Roscoe Road, also known as the Magusi River Road, is the largest logging

road in the area and crosses Tannahill Township 1.6 km’s south of the showing. An over-grown

logging road located at 594998mE, 5362285mN, 300 metres west of the 18 km marker on the

Roscoe Road provides ATV access to the Miron Cu-Ag-Au Occurrence. At approximately 2 km

north along this route, a trail has been cut from the logging road west to the Miron trench on

the Magusi River.

Claim Ownership and Logistics

Mining claim 529540 consists of eight contiguous cells covering a total area of 171.12

hectares (Figure 2). The claim is registered 100% in the name of Brandy Brook Mines Limited

located at 8901 Reily Drive, Mount Brydges, Ontario.

Claim 529540 has an Anniversary Date of: December 15, 2019.

7

Land Status and Topography

Mining claim 529540 is situated entirely on Crown Land. The property is uninhabited

and there are no buildings, structures or electricity. The closest transmission line is

approximately 5 km’s west of the property.

The Miron Cu-Ag-Au Occurrence occurs in an outcrop located on the east side of the

Magusi River. But most of the property is covered by thick overburden consisting of clay and

till. Outcrop exposure is less than 5%. Most outcrops are found along the Magusi River and in

higher elevations.

With the exception of the river valley, most of the property has gentle topography

ranging 285 to 320 metres above sea level. Many areas of the property are flat or gently sloped.

Some areas of the property have been logged at various times within the last 20 years.

Logged areas are situated marginal to the river valley. Logged areas are overgrown with alders

and small poplar trees. Old-growth areas have been left to act as boundaries between logged

areas and the waterways crossing the property. Trees within old-growth areas include: spruce,

pine, poplar, maple, ash and alders.

Geology

The Miron Cu-Ag-Au occurrence is located in the Harker-Holloway section of the Abitibi

Greenstone Belt. The property is underlain by Archean units of the Blake River assemblage

dated 2704 to 2696 Ma.

Exposed outcrops are rare on the property. Outcrops consist mostly of flow and

pillowed basalts, flow breccia and gabbro. Rock units generally trend east-west or trend

northeast-southwest and dip moderately towards the south and southeast.

The Miron Cu-Ag-Au occurrence is hosted by tholeiitic pillowed basalts of the Upper

Blake River assemblage. The unit strikes approximately 1200 with pillow tops orientated

towards the southwest. The unit is crossed by northeast trending fractures striking roughly 400

and dip 560 southeast. Some of the fractures contain quartz-calcite stringers mineralized with

pyrite and chalcopyrite. The main copper bearing minerals in the Miron occurrence include:

chalcopyrite, chalcocite, malachite, azurite and rare native copper (Figure 4). Chalcopyrite,

pyrite and occasionally magnetite occur mostly in the pillow salvages and with quartz-calcite

stringers which cut across the pillows (Figure 4). The mineralization is believed to be part of a

9

volcanogenic massive sulphide (VMS) deposit. Late-stage white calcite stringers barren of

sulphides are superimposed over some sections of the occurrence.

History of Exploration

The Miron Cu-Ag-Au occurrence was discovered in 1986, by prospector Ted Miron of

Sudbury, Ontario. A limited amount of overburden stripping was completed and a gold assay of

0.29 oz/ton was reported from a small pit on the east side of the river (MDI32D05NE00039).

In 1987, the gold occurrence was acquired by prospectors: Ivan Gagne and Andre St.

Amant. They proceeded to strip the overburden, power wash the outcrop and blast several

trenches across the outcrop. Five rock samples are reported to have assayed: 0.002 to 1.26

oz/ton gold, 0.11 to 0.41 oz/ton silver and 1.01 to 3.80% copper (Assessment File

32D05NE0036).

In 1988, Gagne and Amant completed an airborne magnetometer and VLF

electromagnetic (EM) survey over their property. The survey was performed by H. Ferderber

Geophysics Ltd. of Val D’Or, Quebec. The survey was flown at a terrain clearance of 300 feet (91

metres) on flight lines spaced 440 feet (135 metres) apart. Navigation of the survey was aided

by video tracing. Two conductive zones were detected by the survey (Assessment File

32D05NE0039).

Between 1988 and 1992, Gagne and St. Amant drilled nine X-Ray holes. Numerous

intersections of chalcopyrite were noted in the drill logs however no assays are reported.

(Assessment Files: 32D05NE0032, 32D05NE0045, 32D05NE9357, 32D05NE9358)

In 1995, Strike Minerals had an option on the Miron occurrence and completed a

mechanized trenching program on the mineralization. Strike reported assay values ranging:

trace to 583 ppb (0.016 oz/ton) gold, trace to 37.0 ppm (1.01 oz/ton) silver, 287 to 87,100 ppm

(8.71%) copper and 91 to 1,360 ppm (0.136 %) zinc. The property lapsed in 2011.

In 2011, Brandy Brook Mines Limited staked the Miron occurrence with claim 4251297.

Brandy Brook completed ground magnetometer and VLF-EM surveys over the occurrence,

collected rock samples, mapped geology and collected several heavy mineral concentrates from

the Magusi River. The magnetometer survey showed the Miron occurrence coincides with a

northeast trending magnetic “low”. Several northeast trending magnetic features, some with

coincident VLF conductors, were detected proximal to the mineralization. Rock samples

collected at the time from the Miron occurrence assayed: <0.02 to 1.46 g/t gold, 0.5 to 46.8 g/t

silver, 0.007 to 8.61% copper and <0.001 to 0.12% zinc. Heavy mineral concentrates collected in

10

the Magusi River contained abundant pyrite and chalcopyrite grains. Many of the sulphide

grains contained inclusions of sphalerite. A single, large gold grain was present in a sample

collected in the river adjacent to the Miron occurrence and another large gold grain was found

in a sample collected upstream from the mineralization. Chalcopyrite and magnetite grains

coated with malachite were found in a heavy mineral sample taken downstream from the

Miron occurrence.

In 2016, Brandy Brook Mines collected additional rock samples at the Miron Cu-Ag-Au

Occurrence. Several channel cuts were made using a gas powered rock saw. Although sampling

was limited to a small area, best results included an 80 cm cut which averaged 1.7% Cu, 10.9 g/t

Ag, 0.06 g/t Au, 204 ppm Co, 338 ppm Ni, 434 ppm Zn, 2.1 ppm Mo and 97.5 ppm V.

In 2017, Brandy Brook collected soil samples over the area. Two anomalies were

delineated, a northeast-southwest trending anomaly coinciding with the Miron occurrence and

a second anomaly coinciding with magnetic and VLF-EM features situated on the west and

north side of the river.

Survey Dates and Personnel

Additional soil samples were collected on claim 529540 on August 20, 2018 (Figure 3).

The soil samples were collected in one day on August 20, 2018

Soil samples were collected by James Chard of Cordova Mines, Ontario and the author,

Robert Dillman of Mount Brydges, Ontario.

Survey Logistics

A total of 15 soil samples were collected during the project. The sample numbers collect

during 2018 program include: G-80 to G-95 inclusive.

The samples were collected at roughly 20 metre intervals along 2 lines spaced 75 metres

apart. The lines were orientated on a bearing of 1600 – 3400. A ribbon was used to mark each

sample site. The UTM coordinates of each sample site were recorded using a Garmin Rhino GPS

unit.

The samples were collected manually by shovel. All the samples were consistently

collected a depth of 10 to 20 cm below the black humus-organic layer. Each sample was

described and placed in a paper bag specifically designed for soil samples. Large pebbles were

removed by hand during sample collection.

11

The soil samples were sent to AGAT Laboratories for analyses. AGAT Laboratories is

located 5023 McAdam Road in Mississauga, Ontario. All the soil samples were analyzed for 54

elements using an Ethylenediaminetetraactic (EDTA) Cyanide Leach followed by Inductively

Coupled Plasma Mass Spectrometry (ICP-MS) to measure the amount of elements in each

sample.

Assay certificates from AGAT Laboratories are appended to this report.

In order to determine anomalies within the assay results, background values for each

element over the survey area has to be determined. Similar to other surveys, this requires some

data manipulation and calculation of Response Ratios. The first step is to determine the Lower

Quartile for each element in the assay Data Set. The Lower Quartile for elements in the soil

samples collected around the Miron occurrence is present in Table 1. Assay values within the

Data Set falling below the detection limit were consider as 0 and omitted from the calculation

of the Lower Quartile. Once the Lower Quartile is determined, the Response Ratio is calculated

by dividing the assay value of any particular element by the Lower Quartile. Decimal values are

rounded accordingly to make whole numbers. Samples with the highest Response Ratios are

considered anomalous. Geochemistry from rock samples collected in the Miron occurrence

helped distinguish which elements are important (Table 2). These elements include: copper

(Cu), silver (Ag), gold (Au), arsenic (As), cobalt (Co), manganese (Mn), nickel (Ni), lead (Pb),

vanadium (V), zinc (Zn).

Results of Soil Sampling

The Response Ratios for the soil samples collected in 2018 and 2017 are summarized in

Table 3.

The assay results for the 2018 soil samples are generally lower overall and result in

lower Response Ratios compared to 2017 samples. Sample G-87 stands out amongst the 2018

assays and is considered anomalous for most of the elements associated with the Miron Cu-Ag-

Au Occurrence: Ag, Au, Co, Cu and Mn.

The assay results for gold were consistently very low. As a measure of quality control,

the 2018 samples were re-assayed for gold resulting in little difference.

12

Table 1. Lower Quartile Derived from the Assays of Soil Samples collected in 2017 and 2018 from the Miron Showing

ELEMENT Assay Range

Lower Quartile

Gold (Au) 0.1 to 1.2 ppb 0.2

Silver (Ag) 2 to 52 ppb 7.25

Cobalt (Co) 11 to 959 ppb 72.0

Copper (Cu) <10 to 2,070 ppb 354.5

Manganese (Mn) <10 to 14,100 ppb 768.25

Nickel (Ni) <5 to 1,310 ppb 267.75

Lead (Pb) 16 to 1,400 ppb 237.75

Vanadium (V) <0.1 to 1,290 ppb 57.25

Zinc (Zn) <20 to 2,840 ppb 466.0

Table 2. Summary of Rock Samples from the Miron Showing (2017)

Sample Numbers

Location Au ppm

Ag ppm

Co ppm

Cu %

Mn ppm

Ni ppm

Pb ppm

V ppm

Zn ppm

MG-69 to MG-75 593854mE, 5363948mN

0.002 – 0.800

<0.2 - 45.8

36.8 - 310

0.030 - 10.90

233 to 1,550

95.8 to 741

<0.5 to 142.0

77.2 to 121

38.3 to 1,540

13

Table 3. Response Ratios for Soil Samples from the Miron Showing

Sample Number

Location UTM Ag

As Au

Co Cu

Mn Ni

Pb

V

Zn

Total Ag+Au+Cu+ Ni+Pb+Zn

Notes

G-1 529540 32D05J364

593901mE 5363963mN

3 1 1 1 3 2 2 4 1 2 15 25 cm depth. Grey clay.

G-2 529540 32D05J364

593885mE 5363975mN

1 1 0 1 1 2 2 2 4 3 9 Base of hill. Large spruce and poplar.

G-3 529540 32D05J364

593870mE 5363988mN

2 0 0 1 0 0 18 1 2 0 21 25 cm depth. Grey clay.

G-4 529540 32D05J364

593909mE 5363949mN

2 1 2 1 1 2 2 3 1 4 14 Flat. Large spruce and poplar.

G-5 529540 32D05J364

593917mE 5363931mN

2 2 0 1 1 2 2 3 4 2 10 6 metres east of river, 20 cm depth. Reddish brown sandy loam. Large spruce.

G-6 529540 32D05J364

593928mE 5363909mN

2 2 1 2 1 2 2 4 6 2 12 25 cm depth. Grey clay. Mid slope steep, facing west. Large spruce and poplar.

G-7 529540 32D05J364

593939mE 5363893mN

1 2 2 2 2 6 3 5 6 7 20 20 cm depth. Grey clay. Flat. Top of hill. Large spruce and poplar.

G-8 529540 32D05J364

593978mE 5363919mN

1 7 0 1 1 2 1 3 3 3 9 5 metres east of trail. Logged area. 20 cm depth. Grey clay. Flat. Poplar.

G-9 529540 32D05J364

593965mE 5363933mN

2 7 1 7

4

2 4 3 3 18 4 15 Logged area. 20 cm depth.

G-10 529540 32D05J364

593960mE 5363955mN

1 6 1 2 4 3 4 16 4 15 Grey clay. Flat. Poplar.

G-11 529540 32D05J364

593943mE 5363968mN

3 1 1 2 2 2 2 3 2 2 13 Logged area. 20 cm depth.

G-12 529540 32D05J364

593943mE 5363982mN

1 1 0 2 2 1 1 3 2 2 10 Grey clay. Flat. Poplar.

G-13 529540 32D05J364

593928mE 53634007mN

3 2 0 2 1 2 2 2 4 1 9 10 metres east of river, 20 cm depth. Reddish brown sandy loam. Large spruce and poplar.

G-14 529540 32D05J364

593995mE 5363975mN

2 1 2 2 2 7 3 1 0 2 12 Gentle slope west following low wet area. 25 cm depth. Grey clay. Large spruce and poplar.

G-15 529540 32D05J364

594000mE 5363977mN

2 1 0 1 2 2 2 3 1 4 13 Moderate slope northwest beside low area. Grey clay. 20 cm depth. Large spruce and poplar

G-16 529540 32D05J364

594008mE 5363957mN

1 9 2 8 2 5 3 2 23 4 14 Top of slope, logged area, poplar. 20 cm depth. Grey clay.

G-17 529540 32D05J364

594017mE 5363934mN

1 1 0 1 2 3 2 4 3 3 12 Logged area. Flat. 20 cm depth.

G-18 529540 32D05J364

594023mE 5363922mN

2 1 1 1 2 3 2 3 3 2 12 Grey clay. Poplar.

G-19 529540 32D05J364

594068mE 5363937mN

1 1 1 1 1 1 1 1 1 5 10 Gentle slope west. 20 cm depth. Grey clay. Poplar. Trail 5 metres north.

G-20 529540 32D05J364

594063mE 5363956mN


14

Table 3. con’t. Response Ratios for Soil Samples from the Miron Showing

Sample Number

Location UTM Ag

As Au

Co Cu

Mn Ni

Pb

V

Zn


Notes

G-21 529540 32D05J364

594047mE 5363973mN


G-22 529540 32D05J364

594044mE 5363991mN

3 1 1 2 1 2 2 4 5 1 12 Grey clay. Poplar.

G-23 529540 32D05J364

594032mE 5364014mN

1 3 1 3 2 7 2 4 11 3 13 Gentle slope west. 25 cm depth.

G-24 529540 32D05J364

594027mE 5364027mN

2 2 0 2 2 5 2 3 3 2 12 Grey clay. Large spruce and poplar.

G-25 529540 32D05J364

594026mE 5364045mN


G-26 529540 32D05J364

594011mE 5364073mN

1 1 0 4 1 1 1 2 3 1 7 Steep slope west and southwest, river bend. River 10 m southwest. Grey clay. Spruce.

G-27 529540 32D05J364

594011mE 5364090mN

1 1 2 4 2 2 2 4 9 3 14 Steep slope southwest. River 12 m southwest. 20 cm depth. Reddish-brown sandy clay.

G-28 529540 32D05J364

594008mE 5364100mN

1 1 1 2 4 9 4 2 0 2 14 Top of steep slope southwest. 25 cm depth.

G-29 529540 32D05J364

594053mE 5364126mN

2 2 0 4 2 4 3 5 4 2 14 Grey clay. Large spruce. Outcrop 2 m west.

G-30 529540 32D05J364

594065mE 5364110mN

2 1 2 2 2 3 1 2 4 2 11 Slope southwest. River 4 m west. Outcrop 25 m north and between G-27. 20 cm depth Reddish-brown clay.

G-31 529540 32D05J364

594070mE 5364093mN

0 0 0 2 0 1 1 1 1 1 3 River 5 metres west. 25 cm depth. Grey-brown clay. Large spruce.

G-32 529540 32D05J364

594078mE 5364074mN


G-33 529540 32D05J364

594086mE 5364049mN

1 1 0 2 2 4 2 3 7 3 11 Grey clay. Large spruce.

G-34 529540 32D05J364

594097mE 5364040mN

1 4 0 3 2 4 2 3 6 4 11 Flat. 20 cm depth. Dark grey sandy clay. Large poplar and spruce.

G-35 529540 32D05J364

594106mE 5364020mN


G-36 529540 32D05J364

594114mE 5363997mN

3 1 3 0 5 1 2 1 0 2 16 Grey clay. Poplar.

G-37 529540 32D05J364

594116mE 5363981mN


G-38 529540 32D05J364

594125mE 5363961mN

1 1 0 5 2 3 2 5 5 5 15 Grey clay. Poplar.

15


Sample Number

Location UTM Ag

As Au

Co Cu

Mn Ni

Pb

V

Zn


Notes

G-39 529540 32D05J363

593859mE 5363944mN

3 0 3 8 6 12 1 0 0 0 13 Very close to Miron Occurrence. Basalt outcrop with chalcopyrite 3 metres northwest. Grey clay.

G-40 529540 32D05J363

593841mE 5363922mN

2 1 1 3 5 5 5 5 2 2 20 3 metres east of river. Flat. Base of slope. 20 metres southwest of showing. 20 cm depth. Brown clay

G-41 529540 32D05J363

593850mE 5363904mN

1 2 0 3 2 3 1 4 3 2 10 Moderate slope west. 20 cm depth. Grey clay. Large spruce.

G-42 529540 32D05J363

593861mE 5363889mN

2 7 4 7 3 7 4 4 30 5 22 Moderate slope west. 20 cm depth. Grey clay. Large spruce.

G-43 529540 32D05J364

593866mE 5363867mN

2 4 1 5 2 6 2 4 14 3 14 Flat. Large spruce. 20 cm depth. Grey clay.

G-44 529540 32D05J384

593880mE 5363845mN

2 3 1 7 2 8 3 4 20 3 15 Flat. Large spruce. 20 cm depth. Grey clay.

G-45 529540 32D05J383

593861mE 5363794mN

3 2 0 0 2 1 2 1 0 1 9 Ridge between two drainage lows/ creeks. 20 cm depth. Brown clay. Poplar and spruce.

G-46 529540 32D05J383

593852mE 5363813mN

2 5 1 6 2 4 3 4 21 3 15 Ridge between lows/ creeks and river. Flat. 20 cm depth. Grey -brown clay. Large poplar and spruce.

G-47 529540 32D05J383

593838mE 5363829mN

7 1 0 4 3 11 4 2 0 1 14 Moderate slope west. 20 cm depth. Grey-brown clay. Large spruce.

G-48 529540 32D05J383

593839mE 5363842mN

4 0 0 1 2 1 1 0 0 0 7 2 metres east of river on steep slope.

G-49 529540 32D05J364

593883mE 5363921mN

2 8 1 7 3 4 3 4 20 3 17 On top of hill east of Miron occurrence.

G-50 529540 32D05J364

593981mE 5364011mN

1 1 0 1 3 2 2 2 2 1 9 Flat, 25 cm depth, grey clay.

G-51 529540 32D05J364

593956mE 5364059mN

4 1 0 3 3 2 2 4 3 2 15 3 metres east of river, flat, slight bog. 35 cm depth. Reddish-brown sandy clay

G-52 529540 32D05J364

593950mE 5364065mN

4 1 2 1 2 5 2 1 0 2 13 5 metres west of river, flat. Base of east facing moderate slope. 25 cm depth. Grey clay. Large spruce.

G-53 529540 32D05J364

593940mE 5364079mN

2 3 1 4 2 6 2 4 12 4 15 Steep slope east. 20 cm depth. Grey clay. Large spruce.

G-54 529540 32D05J364

593936mE 5364101mN

2 5 1 5 2 4 2 5 13 4 16 Flat. Big spruce. 20 cm depth. Grey clay.

G-55 529540 32D05J364

593928mE 5364110mN

2 12 4 13 3 9 5 6 37 5 25 Gentle slope north. Big spruce. 20 cm depth. Grey clay.

16


Sample Number

Location UTM Ag

As Au

Co Cu

Mn Ni

Pb

V

Zn


Notes

G-56 529540 32D05J364

593891mE 5364094mN

1 1 0 1 0 1 1 1 5 1 4 Gentle slope north. Big spruce. 20 cm depth. Grey clay.

G-57 529540 32D05J364

593902mE 5364077mN

1 5 2 5 2 7 3 4 21 6 18 Flat. Big spruce. 20 cm depth. Grey clay.

G-58 529540 32D05J364

593909mE 5364059mN

1 3 1 4 3 9 3 4 13 6 18 Gentle slope southeast. 8 metres to river. 20 cm depth. Grey clay. Large spruce.

G-59 529540 32D05J364

593919mE 5364034mN

1 6 2 13 2 5 3 4 15 4 16 Gentle to moderate slope southeast. 20 cm depth. Grey-brown clay. Large spruce.

G-60 529540 32D05J364

593868mE 5364016mN

3 0 4 1 5 2 1 4 1 1 18 2 metres west of river, base of steep slope, 20 cm depth, grey clay with pebbles. Spruce.

G-61 529540 32D05J363

593859mE 5364028mN

3 3 3 3 0 0 0 3 0 0 9 Steep slope east just below top. 20 cm grey-brown clay. Large spruce.

G-62 529540 32D05J363

593854mE 5364054mN

1 2 0 2 1 3 2 4 6 4 12 Flat. 20 cm depth. Grey clay. Large poplar and spruce.

G-63 529540 32D05J363

5939850mE 5364069mN


G-64 529540 32D05J363

593790mE 5364030mN


G-65 529540 32D05J363

593800mE 5364011mN

2 6 1 4 2 6 2 5 15 4 16 Gentle slope east. 20 cm depth. Grey clay. Large poplar and spruce.

G-66 529540 32D05J363

593812mE 5363992mN

1 2 1 3 2 4 2 4 10 3 13 Top of hill. 20 cm depth. Grey clay. Large poplar and spruce.

G-67 529540 32D05J363

593825mE 5363975mN

2 4 0 4 3 7 3 4 11 5 17 Steep slope east. 20 cm depth. Grey-brown clay. Large spruce.

G-68 529540 32D05J363

593829mE 5363953mN

2 3 1 5 3 7 5 4 8 5 25 5 metres west of river, flat. Base of slope. 25 cm depth. Grey clay. Large spruce.

G-69 529540 32D05J363

593929mE 5363990mN

1 6 2 9 4 8 4 5 18 4 20 Base of slope 2 metres from river across from Miron Occurrence. 20 cm depth. Grey clay. Large spruce.

G-70 529540 32D05J363

593817mE 5363893mN

2 0 1 1 1 4 3 1 0 0 8 6 metres west of river, flat, flood plain. 45 cm depth. Brown-grey clay. Large spruce, alders.

G-71 529540 32D05J363

593801mE 5363907mN

3 0 6 1 2 3 1 0 0 0 12 Flat, flood plain. 40 cm depth. Grey clay. Large spruce, alders.

G-72 529540 32D05J363

593798mE 5363918mN

2 1 6 2 3 6 2 1 0 3 17 Gentle slope east. 20 cm depth. Grey clay. Spruce and alders.

G-73 529540 32D05J363

593790mE 5363936mN

1 1 0 2 2 18 2 1 0 1 7 3 metres west of river. Flat. 35 cm depth. Dark grey clay and black humus. Spruce, alders.

G-74 529540 32D05J363

593788mE 5363953mN

3 1 2 2 3 2 2 2 0 1 13 Base of moderately steep southeast facing slope. 20 cm depth. Grey clay. Large spruce.

G-75 529540 32D05J363

593781mE 5363973mN

3 3 0 3 2 3 2 4 8 3 14 Top crest of hill. Flat. 20 cm depth. Reddish –brown - grey clay. Large poplar and spruce.

17


Sample Number

Location UTM Ag

As Au

Co Cu

Mn Ni

Pb

V

Zn


Notes

G-76 529540 32D05J363

593768mE 5363997mN

2 1 0 4 1 5 2 3 5 3 11 Flat. 20 cm depth. Reddish–brown-grey clay. Large poplar and spruce.

G-77 529540 32D05J363

593752mE 5364009mN

1 2 0 5 1 5 2 3 11 3 10 Flat. 20 cm depth. Grey clay. Large spruce.

G-78 ------

------

NA NA NA NA NA NA NA NA NA NA NA No sample

G-79 -------

------

NA NA NA NA NA NA NA NA NA NA NA No sample

G-80 529540 32D05J383

593741mE 5363769mN

1 0 0 1 1 2 1 1 1 1 5 Beside river, brown-grey clay. 20 cm

G-81 529540 32D05J383

593719mE 5363791mN

1 1 0 1 1 1 1 1 2 1 5 Steep slope southeast. Light brown clay 15 cm

G-82 529540 32D05J383

593710mE 5363807mN

1 0 0 0 1 1 1 1 1 1 5 Top of hill flat. Light brown clay. 15 cm.

G-83 529540 32D05J363

593697mE 5363826mN

1 0 0 0 1 1 0 1 0 1 4 Flat. Light brown clay. 15 cm.

G-84 529540 32D05J363

593687mE 5363858mN

1 0 0 0 1 1 1 1 1 1 5 Slight slope southeast. Light brown clay. 15 cm.

G-85 529540 32D05J363

593684mE 5363888mN

1 0 0 0 0 0 0 1 1 0 2 Flat. Brown clay. 20 cm

G-86 529540 32D05J363

593679mE 5363903mN

1 1 0 1 1 1 1 1 3 0 4 Flat. Light brown clay. 15 cm

G-87 529540 32D05J363

593672mE 5363926mN

4 0 1 2 2 7 1 0 0 1 9 Steep slope northwest along creek. Brown clay. 15 cm

G-88 529540 32D05J363

593605mE 5363898mN

1 0 1 0 1 1 1 1 1 1 6 Flat. 15 cm humus. Light brown clay. 25 cm

G-89 529540 32D05J363

593610mE 5363878mN

1 0 0 0 1 1 1 1 2 1 5 Flat. 15 cm humus. Light brown clay. 25 cm

G-90 529540 32D05J383

593613mE 5363843mN


G-91 529540 32D05J383

593619mE 5363822mN


G-92 529540 32D05J383

593633mE 5363801mN


G-93 529540 32D05J383

593635mE 5363781mN


G-94 529540 32D05J383

593639mE 5363753mN


G-95 529540 32D05J383

593651mE 5363727mN

1 0 0 0 1 1 1 1 1 1 5 Flat. 20 cm humus. Grey clay. 30 cm

18

Discussion of Results

High Response Ratios for total counts of Au + Ag + Cu + Ni + Pb + Zn concentrations in

the soil samples from the 2017 and 2018 surveys are mostly focused around the Miron Cu-Ag-

Au Occurrence. The soil anomaly branches to the northeast across the river and coincides with

ground magnetic and VLF-EM features situated on the west side of the river. The soil anomaly

also appears to extend south along the east side the river and continues east from the showing

along the side of the river valley. Magnetic and VLF-EM features occur in the vicinity to both of

these trends.

Conclusions and Recommendations

The soil survey results suggest some of the geophysical features in the vicinity to the

Miron Cu-Ag-Au Occurrence could represent additional zones of mineralization. Additional soil

sampling is warranted on these targets prior to drill testing. A Mobile Metal Ionization (MMI)

survey is recommended to verify the soil anomalies and prioritize the geophysical features for

drill testing.

Respectfully Submitted,

Robert J. Dillman P.Geo., B.Sc.

May 17, 2019

19

Robert J. Dillman P.Geo, B.Sc. ARJADEE PROSPECTING

8901 Reily Drive, Mount Brydges, Ontario, Canada, N0L1W0 Phone/ fax (519) 264-9278

CERIFICATE of AUTHOR

I, Robert J. Dillman, Professional Geologist, do certify that: 1. I am the President and the holder of a Certificate of Authorization for: ARJADEE PROSPECTING 8901 Reily Drive Mount Brydges, Ontario, Canada N0L1W0 2. I graduated in 1991 with a Bachelor of Science Degree in Geology at the University of Western Ontario. 3. I am an active member of: Association of Professional Geoscientists of Ontario, APGO Prospectors and Developers Association of Canada, PDAC 4. I have been a licensed Prospector in Ontario since 1985. 5. I have worked continuously as a Professional Geologist for 28 years. 6. I am President and CEO of Brandy Brook Mines Limited 7. Unless stated otherwise, I am responsible for the preparation of all sections of the Assessment Report titled: REPORT ON ADDITIONAL SOIL SAMPLING IN THE VICINITY TO THE MIRON COPPER-SILVER-GOLD OCCURRENCE TANNAHILL TOWNSHIP, LARDER LAKE MINING DIVISION NORTHERN ONTARIO dated, May 17, 2019 8. I am not aware of any material fact or material change with respect to the subject matter of the Assessment Report that is not contained in the Assessment Report and its omission to disclose makes the Assessment Report misleading. Dated this 17th day of May, 2019

20

References

Campbell, R.A. 1988. Report on Combined Airborne Geophysical Survey on the Property of Mr.

Y. Gagne, Tannahill Township, Ontario, by H. Ferderber Geophysics; Unpublished

assessment report 32D05NE0039.

Dillman, R.J. 2011. Report On Ground Magnetometer and VLF-Electromagnetic Surveys GRID A:

Tannahill Property, Tannahill Township, Ontario. Unpublished assessment report. For:

Brandy Brook Mines Limited.

Dillman R.J. 2017. Report On Rock and Soil Sampling, Miron Copper-Silver Occurrence

Claim 4251297, Tannahill Township, Larder Lake Mining Division, Abitibi Greenstone

Belt, Northern Ontario.

Forbes, C.P. 1996. Report on Stripping and Trenching on the Strike Minerals Inc. Tannahill

Township Property, Larder Mining Division. Contains: Report by Alex Bath 1987,

Gagne/St. Amant Prospect Tannahill Township, Larder Lake Mining Division.

Unpublished assessment report 32D05NE0070.

Gagne, Y. 1987. Assay certificates. Gagne - St. Amant Prospect. Unpublished assessment report

32D05NE0036.

Gagne, Y. 1988. X-Ray Drill Logs Holes: 3, 4 & 5. Gagne-St. Amant Prospect. Unpublished


Gagne, Y. 1989. X-Ray Drill Logs Holes: 6 & 7. Gagne - St. Amant Prospect. Unpublished


Gagne, Y. 1991. X-Ray Drill Logs Hole: 8. Gagne-St. Amant Prospect. Unpublished assessment

report 32D05NE9358.

Gagne, Y. 1991. X-Ray Drill Logs Hole: 9. Gagne-St. Amant Prospect. Unpublished assessment

report 32D05NE9357.

Jenson, L.S. 1971. Preliminary Geology Map of Tannahill Township, Cochrane District. For:

Ontario Geological Survey Map: P.706, file P0706.

Jenson, L.S. 1972. Geology Map of Tannahill and Dokis Townships, Cochrane District. For:

Ontario Geological Survey Map: 2367, file M2367.

CLIENT NAME: MISC AGAT CLIENT ON, ON

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DATE REPORTED:

PAGES (INCLUDING COVER): 12

Mar 25, 2019

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Laboratories (V2) Page 1 of 12

All samples are stored at no charge for 90 days. Please contact the lab if you require additional sample storage time.

VERSION 2:Revised Reports issued on March/25/2019. Samples were dried and crushed and then proceeded with EDTA Cyanide Leach for Gold Analysis

*NOTES

Results relate only to the items tested. Results apply to samples as received.

SampleLogin

WeightAnalyte:

kgUnit:

Sample ID (AGAT ID) RDL: 0.01

0.57G-80 (9640758)

0.72G-81 (9640759)

0.64G-82 (9640760)

0.58G-83 (9640761)

0.68G-84 (9640762)

0.54G-85 (9640763)

0.56G-86 (9640764)

0.63G-87 (9640765)

0.76G-88 (9640766)

0.77G-89 (9640767)

0.76G-90 (9640768)

0.68G-91 (9640769)

0.64G-92 (9640770)

0.88G-93 (9640771)

0.74G-94 (9640772)

0.82G-95 (9640773)

RDL - Reported Detection LimitComments:


DATE RECEIVED: Oct 18, 2018

Certificate of Analysis

ATTENTION TO: Robert DillmanCLIENT NAME: MISC AGAT CLIENT ON

AGAT WORK ORDER: 18T398871

(200-) Sample Login Weight

DATE SAMPLED: Oct 21, 2018 DATE REPORTED: Mar 25, 2019 SAMPLE TYPE: Other


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CERTIFICATE OF ANALYSIS (V2)

Certified By:Page 2 of 12

Ag Al As Au Ba Bi Ca CsCe Co CrCdAnalyte: DyCu

ppb ppm ppb ppb ppb ppb ppm ppbppb ppb ppbppbUnit: ppbppb

Sample ID (AGAT ID) RDL: 1 110 0.1 10 1 10 1 5 5 30 0.5 101

7 305 11 <0.1 157 <1 47 1.7300 50 6116G-80 (9640758) 257 104

6 382 12 <0.1 301 <1 49 4.0424 37 1135G-81 (9640759) 165 70

9 263 <10 <0.1 221 <1 134 2.0149 27 908G-82 (9640760) 225 39

4 124 <10 <0.1 136 <1 319 <0.5116 13 855G-83 (9640761) 205 25

9 212 <10 <0.1 192 <1 148 <0.5323 17 498G-84 (9640762) 270 86

4 391 <10 <0.1 109 <1 <10 1.737 20 504G-85 (9640763) 48 13

5 490 19 <0.1 329 1 42 6.6187 72 15711G-86 (9640764) 258 78

30 24 <10 <0.1 115 <1 590 <0.5119 160 <306G-87 (9640765) 612 16

4 181 <10 <0.1 184 <1 213 1.0398 17 1133G-88 (9640766) 302 94

10 393 <10 <0.1 218 <1 16 4.3153 29 1149G-89 (9640767) 151 57

6 372 12 <0.1 243 <1 62 3.5245 38 1199G-90 (9640768) 171 35

8 291 14 <0.1 267 <1 149 3.0186 28 1225G-91 (9640769) 209 33

7 326 14 <0.1 303 <1 118 3.5232 28 1315G-92 (9640770) 214 41

4 178 <10 <0.1 223 <1 174 1.7293 11 766G-93 (9640771) 130 35

4 214 <10 <0.1 148 <1 142 0.9292 22 6316G-94 (9640772) 191 54

5 277 <10 <0.1 155 <1 83 2.2284 24 8610G-95 (9640773) 178 72






(201-999) EDTA Cyanide Leach, ICP-MS finish



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Er Eu Fe Ga Gd Hg In MnLa Li MgKAnalyte: NbMo

ppb ppb ppm ppb ppb ppb ppb ppbppb ppb ppmppmUnit: ppbppb

Sample ID (AGAT ID) RDL: 0.5 0.51 1 1 1 0.5 0.1 1 5 1 10 50.5

53.5 18.8 99 15 97 <1 <0.5 1160108 24 1417.4G-80 (9640758) <5 <0.5

31.4 16.9 143 29 86 <1 <0.5 535174 55 1832.2G-81 (9640759) <5 <0.5

21.0 6.4 117 13 34 <1 <0.5 68058 26 2746.6G-82 (9640760) <5 <0.5

15.9 4.6 45 3 24 <1 <0.5 55359 <5 3947.4G-83 (9640761) <5 <0.5

46.5 17.0 58 10 92 <1 <0.5 767220 <5 2113.9G-84 (9640762) <5 <0.5

13.9 0.9 109 10 5 <1 <0.5 10717 22 49.6G-85 (9640763) <5 <0.5

41.7 10.7 208 33 59 <1 <0.5 65166 99 2926.4G-86 (9640764) <5 6.2

9.9 2.8 2 2 17 <1 <0.5 555011 16 709.3G-87 (9640765) <5 <0.5

54.4 22.0 87 11 109 2 <0.5 480200 12 2715.1G-88 (9640766) <5 <0.5

28.8 8.3 169 25 44 <1 <0.5 58353 58 1323.5G-89 (9640767) <5 <0.5

16.1 8.3 152 24 40 <1 <0.5 77290 47 1822.3G-90 (9640768) <5 <0.5

17.1 6.7 146 19 33 <1 <0.5 54182 41 2924.0G-91 (9640769) <5 1.9

21.9 8.0 171 22 42 <1 <0.5 57498 54 3022.7G-92 (9640770) <5 0.9

18.1 8.4 78 13 41 <1 <0.5 370121 19 2618.2G-93 (9640771) <5 <0.5

28.7 11.9 86 12 61 <1 <0.5 931127 12 1916.5G-94 (9640772) <5 <0.5

36.7 14.2 145 17 73 <1 <0.5 541116 28 1717.4G-95 (9640773) <5 <0.5









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Nd Ni P Pb Pd Pr Pt SmSb Sc SeRbAnalyte: SrSn

ppb ppb ppm ppb ppb ppb ppb ppbppb ppb ppbppbUnit: ppbppb

Sample ID (AGAT ID) RDL: 1 100.1 10 1 1 1 5 1 5 2 1 15

330 265 2.8 217 109 66 <1 79<1 117 2269G-80 (9640758) <1 124

361 160 2.8 248 52 82 <1 77<1 107 23116G-81 (9640759) <1 90

114 218 1.3 224 208 24 <1 27<1 72 2184G-82 (9640760) <1 192

84 95 0.4 136 381 18 <1 20<1 69 2149G-83 (9640761) <1 300

391 196 0.5 229 268 83 <1 76<1 153 2249G-84 (9640762) <1 235

19 77 1.7 117 <1 5 <1 4<1 48 1970G-85 (9640763) <1 14

164 247 1.7 310 105 32 3 44<1 203 23157G-86 (9640764) <1 126

32 238 0.1 60 441 5 <1 11<1 11 2021G-87 (9640765) <1 377

396 183 0.5 165 176 83 <1 98<1 123 2160G-88 (9640766) <1 183

119 164 6.2 231 <1 24 3 33<1 115 24122G-89 (9640767) <1 37

159 147 4.9 243 35 35 <1 35<1 78 22111G-90 (9640768) <1 88

122 140 1.9 232 207 27 <1 29<1 95 2097G-91 (9640769) <1 196

154 177 1.9 236 192 34 <1 34<1 95 24108G-92 (9640770) <1 197

182 152 3.0 115 138 43 2 38<1 67 2281G-93 (9640771) <1 159

241 178 1.4 175 118 53 <1 55<1 97 2259G-94 (9640772) <1 137

256 199 3.0 158 50 54 <1 62<1 82 2282G-95 (9640773) <1 104









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Ta Tb Th Ti Tl U V ZrY Yb ZnWAnalyte:

ppb ppb ppb ppb ppb ppb ppb ppbppb ppb ppbppbUnit:

Sample ID (AGAT ID) RDL: 1 0.5 3 0.5 1 1 1 1 1 20 51

<1 16 82.6 2090 <0.5 8 59 101512 40 450<1G-80 (9640758)

<1 13 110 4310 <0.5 10 97 237349 22 260<1G-81 (9640759)

<1 6 74.6 1890 <0.5 12 57 130249 16 621<1G-82 (9640760)

<1 4 43.9 117 <0.5 12 5 69170 13 457<1G-83 (9640761)

<1 14 62.2 863 <0.5 11 30 79485 37 466<1G-84 (9640762)

<1 1 37.2 1960 <0.5 4 40 9383 13 108<1G-85 (9640763)

<1 11 128 7430 <0.5 11 198 287415 31 350<1G-86 (9640764)

<1 2 17.6 7 <0.5 1 4 8117 9 110<1G-87 (9640765)

<1 16 81.3 1150 <0.5 29 28 109432 46 213<1G-88 (9640766)

<1 8 80.7 4220 <0.5 7 97 203336 22 417<1G-89 (9640767)

<1 6 84.9 5650 <0.5 6 107 202198 12 553<1G-90 (9640768)

<1 5 96.5 5210 <0.5 13 131 245207 14 466<1G-91 (9640769)

<1 7 90.6 4930 <0.5 13 139 240278 17 340<1G-92 (9640770)

<1 6 80.7 2490 <0.5 7 49 156210 15 235<1G-93 (9640771)

<1 9 81.0 2380 <0.5 10 54 136344 23 430<1G-94 (9640772)

<1 12 79.5 2360 <0.5 12 62 158349 27 350<1G-95 (9640773)










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AuAnalyte:

ppbUnit:


<0.1G-80 (9640758)

<0.1G-81 (9640759)

<0.1G-82 (9640760)

<0.1G-83 (9640761)

<0.1G-84 (9640762)

<0.1G-85 (9640763)

<0.1G-86 (9640764)

0.1G-87 (9640765)

0.1G-88 (9640766)

<0.1G-89 (9640767)

<0.1G-90 (9640768)

<0.1G-91 (9640769)

0.1G-92 (9640770)

<0.1G-93 (9640771)

<0.1G-94 (9640772)

<0.1G-95 (9640773)







(201-999) EDTA Cyanide Leach, ICP-MS finish - Au, After Drying and Crushing



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REPLICATE #1 REPLICATE #2

Parameter Sample ID Original Replicate RPD Sample ID Original Replicate RPD

Ag 9640758 7 15 9640769 8 7 13.3%

Al 9640758 305 314 2.9% 9640769 291 263 10.1%

As 9640758 11 < 10 9640769 14 10

Au 9640758 < 0.1 < 0.1 0.0% 9640769 < 0.1 < 0.1 0.0%

Ba 9640758 157 151 3.9% 9640769 267 220 19.3%

Bi 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Ca 9640758 47 46 2.2% 9640769 149 139 6.9%

Cd 9640758 16 17 6.1% 9640769 5 5 0.0%

Ce 9640758 300 336 11.3% 9640769 186 205 9.7%

Co 9640758 50 47 6.2% 9640769 28 22 24.0%

Cr 9640758 61 52 15.9% 9640769 122 106 14.0%

Cs 9640758 1.7 1.6 6.1% 9640769 3.0 1.7

Cu 9640758 257 269 4.6% 9640769 209 172 19.4%

Dy 9640758 104 107 2.8% 9640769 33 36 8.7%

Er 9640758 53.5 53.1 0.8% 9640769 17.1 18.2 6.2%

Eu 9640758 18.8 20.1 6.7% 9640769 6.7 7.4 9.9%

Fe 9640758 99 92 7.3% 9640769 146 126 14.7%

Ga 9640758 15 15 0.0% 9640769 19 14

Gd 9640758 97 104 7.0% 9640769 33 38 14.1%

Hg 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

In 9640758 < 0.5 < 0.5 0.0% 9640769 < 0.5 < 0.5 0.0%

K 9640758 17.4 16.6 4.7% 9640769 24.0 18.6 25.4%

La 9640758 108 116 7.1% 9640769 82 86 4.8%

Li 9640758 24 23 4.3% 9640769 41 30 31.0%

Mg 9640758 14 14 0.0% 9640769 29 22 27.5%

Mn 9640758 1160 887 26.7% 9640769 541 485 10.9%

Mo 9640758 < 5 6 9640769 < 5 < 5 0.0%

Nb 9640758 < 0.5 < 0.5 0.0% 9640769 1.9 < 0.5

Nd 9640758 330 359 8.4% 9640769 122 140 13.7%

Ni 9640758 265 258 2.7% 9640769 140 135 3.6%

P 9640758 2.8 2.7 3.6% 9640769 1.9 1.7 11.1%


CLIENT NAME: MISC AGAT CLIENT ON ATTENTION TO: Robert Dillman



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QUALITY ASSURANCE REPORT Page 8 of 12

Pb 9640758 217 225 3.6% 9640769 232 228 1.7%

Pd 9640758 109 83 27.1% 9640769 207 204 1.5%

Pr 9640758 66 73 10.1% 9640769 27 31 13.8%

Pt 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Rb 9640758 69 66 4.4% 9640769 97 85 13.2%

Sb 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Sc 9640758 117 115 1.7% 9640769 95 77 20.9%

Se 9640758 22 22 0.0% 9640769 20 19 5.1%

Sm 9640758 79 88 10.8% 9640769 29 33 12.9%

Sn 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Sr 9640758 124 118 5.0% 9640769 196 173 12.5%

Ta 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Tb 9640758 16 17 6.1% 9640769 5 6 18.2%

Th 9640758 82.6 78.6 5.0% 9640769 96.5 88.9 8.2%

Ti 9640758 2090 1760 17.1% 9640769 5210 3980 26.8%

Tl 9640758 < 0.5 < 0.5 0.0% 9640769 < 0.5 < 0.5 0.0%

U 9640758 8 7 13.3% 9640769 13 11 16.7%

V 9640758 59 47 22.6% 9640769 131 112 15.6%

W 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Y 9640758 512 537 4.8% 9640769 207 223 7.4%

Yb 9640758 40 40 0.0% 9640769 14 15 6.9%

Zn 9640758 450 478 6.0% 9640769 466 416 11.3%

Zr 9640758 101 93 8.2% 9640769 245 219 11.2%




Au 9640758 < 0.1 < 0.1 0.0% 9640769 < 0.1 < 0.1 0.0%







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CRM #1 (ref.SOIL)

Parameter Expect Actual Recovery Limits

Au 0.168 0.217 129% 80% - 120%





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Solid Analysis

Sample Login Weight MIN-12009 BALANCE

Ag ICP/MS

Al ICP/MS

As ICP/MS

Au ICP/MS

Ba ICP/MS

Bi ICP-MS

Ca ICP/MS

Cd ICP-MS

Ce ICP-MS

Co ICP/MS

Cr ICP/MS

Cs ICP-MS

Cu ICP/MS

Dy ICP-MS

Er ICP-MS

Eu ICP-MS

Fe ICP/MS

Ga ICP-MS

Gd ICP-MS

Hg ICP/MS

In ICP-MS

K ICP/MS

La ICP-MS

Li ICP/MS

Mg ICP/MS

Mn ICP/MS

Mo ICP/MS

Nb ICP-MS

Nd ICP-MS

Ni ICP/MS

P ICP/MS

Pb ICP/MS

Pd ICP/MS

Pr ICP-MS

Pt ICP/MS

Rb ICP/MS

Sb ICP-MS

Sc ICP/OES

Se ICP/MS

Sm ICP-MS

Sn ICP/MS

Sr ICP-OES

Ta ICP-MS

Tb ICP-MS

Th ICP-MS

Ti ICP/MS

Tl ICP-MS

U ICP-MS


SAMPLING SITE: SAMPLED BY:


Method Summary


CLIENT NAME: MISC AGAT CLIENT ON


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METHOD SUMMARY (V2) Page 11 of 12

V ICP/MS

W ICP-MS

Y ICP-MS

Yb ICP-MS

Zn ICP/MS

Zr ICP-MS




Method Summary





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CLIENT NAME: MISC AGAT CLIENT ON, ON

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Kevin Motomura, Data Review SupervisorSOLID ANALYSIS REVIEWED BY:

DATE REPORTED:

PAGES (INCLUDING COVER): 11

Dec 03, 2018

Should you require any information regarding this analysis please contact your client services representative at (905) 501-9998

18T398871AGAT WORK ORDER:



Laboratories (V1) Page 1 of 11

All samples are stored at no charge for 90 days. Please contact the lab if you require additional sample storage time.

*NOTES

Results relate only to the items tested and to all the items tested

SampleLogin

WeightAnalyte:

kgUnit:


0.57G-80 (9640758)

0.72G-81 (9640759)

0.64G-82 (9640760)

0.58G-83 (9640761)

0.68G-84 (9640762)

0.54G-85 (9640763)

0.56G-86 (9640764)

0.63G-87 (9640765)

0.76G-88 (9640766)

0.77G-89 (9640767)

0.76G-90 (9640768)

0.68G-91 (9640769)

0.64G-92 (9640770)

0.88G-93 (9640771)

0.74G-94 (9640772)

0.82G-95 (9640773)







(200-) Sample Login Weight

DATE SAMPLED: Oct 21, 2018 DATE REPORTED: Dec 03, 2018 SAMPLE TYPE: Other


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Ag Al As Au Ba Bi Ca CsCe Co CrCdAnalyte: DyCu

ppb ppm ppb ppb ppb ppb ppm ppbppb ppb ppbppbUnit: ppbppb

Sample ID (AGAT ID) RDL: 1 110 0.1 10 1 10 1 5 5 30 0.5 101

7 305 11 <0.1 157 <1 47 1.7300 50 6116G-80 (9640758) 257 104

6 382 12 <0.1 301 <1 49 4.0424 37 1135G-81 (9640759) 165 70

9 263 <10 <0.1 221 <1 134 2.0149 27 908G-82 (9640760) 225 39

4 124 <10 <0.1 136 <1 319 <0.5116 13 855G-83 (9640761) 205 25

9 212 <10 <0.1 192 <1 148 <0.5323 17 498G-84 (9640762) 270 86

4 391 <10 <0.1 109 <1 <10 1.737 20 504G-85 (9640763) 48 13

5 490 19 <0.1 329 1 42 6.6187 72 15711G-86 (9640764) 258 78

30 24 <10 <0.1 115 <1 590 <0.5119 160 <306G-87 (9640765) 612 16

4 181 <10 <0.1 184 <1 213 1.0398 17 1133G-88 (9640766) 302 94

10 393 <10 <0.1 218 <1 16 4.3153 29 1149G-89 (9640767) 151 57

6 372 12 <0.1 243 <1 62 3.5245 38 1199G-90 (9640768) 171 35

8 291 14 <0.1 267 <1 149 3.0186 28 1225G-91 (9640769) 209 33

7 326 14 <0.1 303 <1 118 3.5232 28 1315G-92 (9640770) 214 41

4 178 <10 <0.1 223 <1 174 1.7293 11 766G-93 (9640771) 130 35

4 214 <10 <0.1 148 <1 142 0.9292 22 6316G-94 (9640772) 191 54

5 277 <10 <0.1 155 <1 83 2.2284 24 8610G-95 (9640773) 178 72









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Er Eu Fe Ga Gd Hg In MnLa Li MgKAnalyte: NbMo

ppb ppb ppm ppb ppb ppb ppb ppbppb ppb ppmppmUnit: ppbppb

Sample ID (AGAT ID) RDL: 0.5 0.51 1 1 1 0.5 0.1 1 5 1 10 50.5

53.5 18.8 99 15 97 <1 <0.5 1160108 24 1417.4G-80 (9640758) <5 <0.5

31.4 16.9 143 29 86 <1 <0.5 535174 55 1832.2G-81 (9640759) <5 <0.5

21.0 6.4 117 13 34 <1 <0.5 68058 26 2746.6G-82 (9640760) <5 <0.5

15.9 4.6 45 3 24 <1 <0.5 55359 <5 3947.4G-83 (9640761) <5 <0.5

46.5 17.0 58 10 92 <1 <0.5 767220 <5 2113.9G-84 (9640762) <5 <0.5

13.9 0.9 109 10 5 <1 <0.5 10717 22 49.6G-85 (9640763) <5 <0.5

41.7 10.7 208 33 59 <1 <0.5 65166 99 2926.4G-86 (9640764) <5 6.2

9.9 2.8 2 2 17 <1 <0.5 555011 16 709.3G-87 (9640765) <5 <0.5

54.4 22.0 87 11 109 2 <0.5 480200 12 2715.1G-88 (9640766) <5 <0.5

28.8 8.3 169 25 44 <1 <0.5 58353 58 1323.5G-89 (9640767) <5 <0.5

16.1 8.3 152 24 40 <1 <0.5 77290 47 1822.3G-90 (9640768) <5 <0.5

17.1 6.7 146 19 33 <1 <0.5 54182 41 2924.0G-91 (9640769) <5 1.9

21.9 8.0 171 22 42 <1 <0.5 57498 54 3022.7G-92 (9640770) <5 0.9

18.1 8.4 78 13 41 <1 <0.5 370121 19 2618.2G-93 (9640771) <5 <0.5

28.7 11.9 86 12 61 <1 <0.5 931127 12 1916.5G-94 (9640772) <5 <0.5

36.7 14.2 145 17 73 <1 <0.5 541116 28 1717.4G-95 (9640773) <5 <0.5









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Nd Ni P Pb Pd Pr Pt SmSb Sc SeRbAnalyte: SrSn

ppb ppb ppm ppb ppb ppb ppb ppbppb ppb ppbppbUnit: ppbppb

Sample ID (AGAT ID) RDL: 1 100.1 10 1 1 1 5 1 5 2 1 15

330 265 2.8 217 109 66 <1 79<1 117 2269G-80 (9640758) <1 124

361 160 2.8 248 52 82 <1 77<1 107 23116G-81 (9640759) <1 90

114 218 1.3 224 208 24 <1 27<1 72 2184G-82 (9640760) <1 192

84 95 0.4 136 381 18 <1 20<1 69 2149G-83 (9640761) <1 300

391 196 0.5 229 268 83 <1 76<1 153 2249G-84 (9640762) <1 235

19 77 1.7 117 <1 5 <1 4<1 48 1970G-85 (9640763) <1 14

164 247 1.7 310 105 32 3 44<1 203 23157G-86 (9640764) <1 126

32 238 0.1 60 441 5 <1 11<1 11 2021G-87 (9640765) <1 377

396 183 0.5 165 176 83 <1 98<1 123 2160G-88 (9640766) <1 183

119 164 6.2 231 <1 24 3 33<1 115 24122G-89 (9640767) <1 37

159 147 4.9 243 35 35 <1 35<1 78 22111G-90 (9640768) <1 88

122 140 1.9 232 207 27 <1 29<1 95 2097G-91 (9640769) <1 196

154 177 1.9 236 192 34 <1 34<1 95 24108G-92 (9640770) <1 197

182 152 3.0 115 138 43 2 38<1 67 2281G-93 (9640771) <1 159

241 178 1.4 175 118 53 <1 55<1 97 2259G-94 (9640772) <1 137

256 199 3.0 158 50 54 <1 62<1 82 2282G-95 (9640773) <1 104









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Ta Tb Th Ti Tl U V ZrY Yb ZnWAnalyte:

ppb ppb ppb ppb ppb ppb ppb ppbppb ppb ppbppbUnit:

Sample ID (AGAT ID) RDL: 1 0.5 3 0.5 1 1 1 1 1 20 51

<1 16 82.6 2090 <0.5 8 59 101512 40 450<1G-80 (9640758)

<1 13 110 4310 <0.5 10 97 237349 22 260<1G-81 (9640759)

<1 6 74.6 1890 <0.5 12 57 130249 16 621<1G-82 (9640760)

<1 4 43.9 117 <0.5 12 5 69170 13 457<1G-83 (9640761)

<1 14 62.2 863 <0.5 11 30 79485 37 466<1G-84 (9640762)

<1 1 37.2 1960 <0.5 4 40 9383 13 108<1G-85 (9640763)

<1 11 128 7430 <0.5 11 198 287415 31 350<1G-86 (9640764)

<1 2 17.6 7 <0.5 1 4 8117 9 110<1G-87 (9640765)

<1 16 81.3 1150 <0.5 29 28 109432 46 213<1G-88 (9640766)

<1 8 80.7 4220 <0.5 7 97 203336 22 417<1G-89 (9640767)

<1 6 84.9 5650 <0.5 6 107 202198 12 553<1G-90 (9640768)

<1 5 96.5 5210 <0.5 13 131 245207 14 466<1G-91 (9640769)

<1 7 90.6 4930 <0.5 13 139 240278 17 340<1G-92 (9640770)

<1 6 80.7 2490 <0.5 7 49 156210 15 235<1G-93 (9640771)

<1 9 81.0 2380 <0.5 10 54 136344 23 430<1G-94 (9640772)

<1 12 79.5 2360 <0.5 12 62 158349 27 350<1G-95 (9640773)










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Ag 9640758 7 15 9640769 8 7 13.3%

Al 9640758 305 314 2.9% 9640769 291 263 10.1%

As 9640758 11 < 10 9640769 14 10

Au 9640758 < 0.1 < 0.1 0.0% 9640769 < 0.1 < 0.1 0.0%

Ba 9640758 157 151 3.9% 9640769 267 220 19.3%

Bi 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Ca 9640758 47 46 2.2% 9640769 149 139 6.9%

Cd 9640758 16 17 6.1% 9640769 5 5 0.0%

Ce 9640758 300 336 11.3% 9640769 186 205 9.7%

Co 9640758 50 47 6.2% 9640769 28 22 24.0%

Cr 9640758 61 52 15.9% 9640769 122 106 14.0%

Cs 9640758 1.7 1.6 6.1% 9640769 3.0 1.7

Cu 9640758 257 269 4.6% 9640769 209 172 19.4%

Dy 9640758 104 107 2.8% 9640769 33 36 8.7%

Er 9640758 53.5 53.1 0.8% 9640769 17.1 18.2 6.2%

Eu 9640758 18.8 20.1 6.7% 9640769 6.7 7.4 9.9%

Fe 9640758 99 92 7.3% 9640769 146 126 14.7%

Ga 9640758 15 15 0.0% 9640769 19 14

Gd 9640758 97 104 7.0% 9640769 33 38 14.1%

Hg 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

In 9640758 < 0.5 < 0.5 0.0% 9640769 < 0.5 < 0.5 0.0%

K 9640758 17.4 16.6 4.7% 9640769 24.0 18.6 25.4%

La 9640758 108 116 7.1% 9640769 82 86 4.8%

Li 9640758 24 23 4.3% 9640769 41 30 31.0%

Mg 9640758 14 14 0.0% 9640769 29 22 27.5%

Mn 9640758 1160 887 26.7% 9640769 541 485 10.9%

Mo 9640758 < 5 6 9640769 < 5 < 5 0.0%

Nb 9640758 < 0.5 < 0.5 0.0% 9640769 1.9 < 0.5

Nd 9640758 330 359 8.4% 9640769 122 140 13.7%

Ni 9640758 265 258 2.7% 9640769 140 135 3.6%

P 9640758 2.8 2.7 3.6% 9640769 1.9 1.7 11.1%







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Pb 9640758 217 225 3.6% 9640769 232 228 1.7%

Pd 9640758 109 83 27.1% 9640769 207 204 1.5%

Pr 9640758 66 73 10.1% 9640769 27 31 13.8%

Pt 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Rb 9640758 69 66 4.4% 9640769 97 85 13.2%

Sb 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Sc 9640758 117 115 1.7% 9640769 95 77 20.9%

Se 9640758 22 22 0.0% 9640769 20 19 5.1%

Sm 9640758 79 88 10.8% 9640769 29 33 12.9%

Sn 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Sr 9640758 124 118 5.0% 9640769 196 173 12.5%

Ta 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Tb 9640758 16 17 6.1% 9640769 5 6 18.2%

Th 9640758 82.6 78.6 5.0% 9640769 96.5 88.9 8.2%

Ti 9640758 2090 1760 17.1% 9640769 5210 3980 26.8%

Tl 9640758 < 0.5 < 0.5 0.0% 9640769 < 0.5 < 0.5 0.0%

U 9640758 8 7 13.3% 9640769 13 11 16.7%

V 9640758 59 47 22.6% 9640769 131 112 15.6%

W 9640758 < 1 < 1 0.0% 9640769 < 1 < 1 0.0%

Y 9640758 512 537 4.8% 9640769 207 223 7.4%

Yb 9640758 40 40 0.0% 9640769 14 15 6.9%

Zn 9640758 450 478 6.0% 9640769 466 416 11.3%

Zr 9640758 101 93 8.2% 9640769 245 219 11.2%







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Parameter





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Solid Analysis

Sample Login Weight MIN-12009 BALANCE

Ag ICP/MS

Al ICP/MS

As ICP/MS

Au ICP/MS

Ba ICP/MS

Bi ICP-MS

Ca ICP/MS

Cd ICP-MS

Ce ICP-MS

Co ICP/MS

Cr ICP/MS

Cs ICP-MS

Cu ICP/MS

Dy ICP-MS

Er ICP-MS

Eu ICP-MS

Fe ICP/MS

Ga ICP-MS

Gd ICP-MS

Hg ICP/MS

In ICP-MS

K ICP/MS

La ICP-MS

Li ICP/MS

Mg ICP/MS

Mn ICP/MS

Mo ICP/MS

Nb ICP-MS

Nd ICP-MS

Ni ICP/MS

P ICP/MS

Pb ICP/MS

Pd ICP/MS

Pr ICP-MS

Pt ICP/MS

Rb ICP/MS

Sb ICP-MS

Sc ICP/OES

Se ICP/MS

Sm ICP-MS

Sn ICP/MS

Sr ICP-OES

Ta ICP-MS

Tb ICP-MS

Th ICP-MS

Ti ICP/MS

Tl ICP-MS

U ICP-MS




Method Summary





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V ICP/MS

W ICP-MS

Y ICP-MS

Yb ICP-MS

Zn ICP/MS

Zr ICP-MS




Method Summary





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