Evaluation of the Meston Lake Property NTS 53 J/4 Meston Lake · which rim of the Superior...

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Evaluation of the Meston Lake Property

NTS 53 J/4

Meston Lake

Red Lake Mining District, Ontario

Reporting Period: September, 2010

A Report for Northern Superior Resources Inc.

Prepared by:

R. Avery, P.Geo. January, 2011

File: Meston_assmnt_rpt.docx

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SUMMARY

During September 2010, geological mapping (1 manday) accompanied by prospecting (4 samples) was undertaken on the Northern Superior Resources Inc.'s wholly owned Meston Lake property located in northwestern Ontario.

The Meston Lake area is part of the underexplored Black Bear Greenstone Belt, bounded by the regionally extensive Stuii-Wunnumin Fault Zone (SWFZ) and its splays, which feature several structural similarities and comparative hydrothermal alteration analogous to large gold deposits in the prolific Abitibi and Red Lake camps elsewhere in the Superior Province.

KEYWORDS

Northwestern Ontario, Superior Province, Sachigo Subprovince, Oxford-Stull Lake terrain, Stuii-Wunnumin Fault, Meston Lake, gold mineralization, hydrothermal alteration, geological mapping, prospecting, fire assay, ICP analyses.

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TABLE OF CONTENTS

1.0 INTRODUCTION 1.1 Location, Access and Physiography 1.2 Dispositions and Ownership

2.0 GEOLOGY 2.1 Previous Mapping 2.2 Regional Geology 2.3 Meston Lake Property Geology 2.4 Quaternary Geology

3.0 ECONOMIC GEOLOGY

4.0 PREVIOUS INVESTIGATIONS

5.0 INVESTIGATIONS 5.1 Geological Mapping 5.2 Fire Assay 5.3 Multi-Element ICP Analysis

6.0 RESULTS 6.1 Geological Mapping - Meston Lake Property 6.2 Prospecting - Meston Lake Property

7.0 CONCLUSIONS AND RECOMMENDATIONS 7.1 Recommendations

8.0 PERSONNEL

9.0 EXPENDITURES

10.0 REFERENCES

11.0 STATEMENT OF QUALIFICATIONS

LIST OF TABLES

Table 1: Table of Dispositions- Meston Lake Property. Table 2: Table of Investigations- 2010 Meston Lake Exploration. Table 3: Statistical Summary of ICP and Gold Analyses - Meston Lake Samples. Table 4: Exploration Expenditures- 2010 Meston Lake Work Program.

LIST OF FIGURES

Figure 1: Project Location Map. Figure 2: Meston Lake Claim Locations. Figure 3: Tectonostratigraphic Components of the Northwest Superior Province.

ii Northern Superior Resources Inc. Evaluation of the Meston Lake Property

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Figure 4: Meston Lake Property Geology. Figure 5: Surficial Geology of Northwestern Ontario. Figure 6: Association of Gold Deposits and Regional Faults- Abitibi Greenstone Belt.

LIST OF MAPS

Map 1: Meston Lake Property Evaluation and Rock Sample Locations.

Appendix 1: Appendix 2 Appendix 3:

LIST OF APPENDICES

Meston Lake Sample Descriptions Certificates of Analysis- Saskatchewan Research Council Manday Distribution - 2010 Meston Lake Exploration

iii Northern Superior Resources Inc. Evaluation of the Meston Lake Property

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1.0 INTRODUCTION

The Meston Lake gold prospect is located in northwestern Ontario approximately 60 kilometres north-northeast of the First Nations community of Sachigo Lake. A helicopter supported reconnaissance evaluation program consisting of geological mapping and sampling was undertaken on the property during September 2010.

1.1 Location, Access and Physiography

The Meston Lake property is centred at latitude 54° 16'N and longitude 91° 45'W (NTS mapsheet 53 J/4) within the Red Lake Mining District of northwestern Ontario. Owing to the absence of aircraft accessible lakes in the immediate area, the prospect is best accessed by helicopter from the First Nations community of Sachjgo Lake, located approximately 60 km to the south-southwest (Figure 1 ).

Sachigo Lake has no year-round road access and is accessible only by air. The community is serviced by a 3500' gravel airstrip with daily air service to Sioux Lookout, Thunder Bay and Winnipeg. During the winter months, the community receives the majority of heavy freight, diesel oil and non-perishable foodstuffs via a winter road which originates in Pickle Lake.

Sachigo Lake is a member of the Windigo First Nations Council and Nishnawbe Aski Nation. Approximately 450 persons reside in the community which features a nursing station, schools and stores for provisioning.

Lodging and accommodation during the field evaluation were provided by the Sachigo Lake First Nation from its Echoing Lake Lodge which is located at the south end of Echoing Lake approximately 35 km west of the Meston Lake property (Figure 1).

The topography of the Meston Lake area is similar to other glaciated portions of the Canadian Shield wherein low rolling hills are frequently interspersed with numerous lakes and swamps. The topography and regional drainage of the area is extremely subdued and slopes gently towards the north. The regional drainage is northward through the Stull, Echoing and Sachigo rivers which merge with the Gods and Severn rivers flowing into Hudson Bay.

Outcrop exposure throughout the Meston Lake area is seen to be very sparse (5-1 0%) and is largely limited to the shores of larger lakes. Till cover and glaciolacustrine clays are extensive across the project area, with large tracts covered by mature stands of pine, spruce, poplar and birch typical of that of a coniferous boreal forest. Cedar, alder and tamarack predominate in more swampy areas. Evidence of recurring forest fires is plainly seen everywhere, with most of the work area having been exposed to intense burning within the last eight to ten years.

The climate of northwestern Ontario is classified as a cold temperate continental climate. On average, Sachigo Lake receives only 145 frost free days each year. The warmest month is July with an avere~ge daily temperature of 16.2°C. The coldest month is January with an average daily temperature of -23. 7°C. On average, Sachigo Lake receives 609 mm of precipitation each year, 37% of which is received as snowfall. Snow begins to accumulate in the area during October each year and generally persists into April. Lakes in the work area are generally frozen over between December and May.

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1.2 Dispositions and Ownership

As summarized in Table 1 and shown in Figure 2, the Meston Lake project area consists of four contiguous claims arrayed in a single rectangular block. Each claim consists of 16 units. Annual assessment requirements on the claims are $25,600.00 per annum.

Table 1: Table of Dispositions - Meston Lake Property.

Claim Number Geographic Anniversary Expenditure Number of Units Location Date Requirement

4250851 16 Hanson River Area 9/16/2011 $6,400.00

4250852 16 Matthews Lake Area 9/16/2011 $6,400.00

4250853 16 Winters Lake Area 9/16/2011 $6,400.00

4250854 16 Fran9ois Lake Area 9/16/2011 $6,400.00

Total 64 $25,600.00

All of the claims are 100% owned by Northern Superior Resources Inc. and are unencumbered.

2.0 GEOLOGY

2.1 Previous Mapping

In 1936, V.B. Meen, J. Satterly and D.L. Downie working variously for the Ontario Department of Mines and Geological Survey of Canada completed the first reconnaissance scale (1 "=2 mile) geological mapping in the region in an easterly arc extending from Stull Lake to the Sachigo River, and as far south as Sachigo Lake. The area was revisited in the late 1960's as part of the Ontario Department of Mines Operation Lingman Lake (Bennett and Riley, 1969) when a 20,000 square mile area of northwestern Ontario was mapped at a scale of I inch to 2 miles.

More recently, the Meston Lake area has been the focus of a collaborative mapping project undertaken by the Ontario Geological Survey, Manitoba Geological Survey and Geological Survey of Canada (Stone eta!., 2001; Skulski eta/., 2000; Davis and Stott, 2001 ). From 1995-2001, the joint federal-provincial NATMAP initiative conducted regional geological mapping concurrent with sampling and analysis of material for lithogeochemistry, thermobarometry and isotopic and geochronological studies over a 12,000 km2 area across the northern Superior Province. The bedrock mapping was focused primarily within a 120 km long, north-south transect across a series of eastsoutheast trending greenstone belts interspersed with plutonic areas and major faults which rim of the Superior Province.

2.2 Regional Geology

The Meston Lake property is located within the Sachigo Subprovince of the Archean Superior Province. As seen in Figure 3, the Sachigo Subprovince is comprised of the North Caribou terrane and Northern Superior superterrane along with intervening

Northern Superior Resources Inc. Evaluation of the Meston Lake Property

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accreted Munroe Lake and Oxford Lake - Stull Lake terranes. To the south, the subprovince is bounded by the Berens River and Uchi subprovinces which comprise felsic plutonic and greenstone dominated terranes respectively (Skulski eta/., 2000). To the northwest, the Sachigo Subprovince terminates against the Pikwitonei granulite terrane which is transitional to the early Proterozoic Trans-Hudson Orogeny. To the north and east, the Sachigo terrrane is overlain by Paleozoic platform strata of the Hudson Bay Lowlands (Figure 3).

In northern Ontario and Manitoba, the Sachigo Subprovince is transected by the StuiiWunnumin Fault Zone (SWFZ), a northwest trending transcrustal megafault (Stott, 1990) which extends for over 600 km from north of Lansdowne House, Ontario to Oxford Lake, Manitoba. In regional airborne magnetic coverage, the Stuii-Wunnumin Fault is characterized by a linear magnetic low that closely follows the margins of a successive series of greenstone belts, including the Bartman-Lavoie, Peeagwon, Wunnumin, Big Trout, Swan Lake, Stull Lake and God's Lake belts. The linear magnetic fabrics of the greenstone belts are seen to curve clockwise into parallelism with the main break on the northeast side of the Stuii-Wunnumin Fault, indicating dextral movement (Osmani eta/., 1989). Aeromagnetic interpretation and outcrop mapping indicate that the SWFZ comprises a 2-5 kilometre wide strike-slip duplex containing numerous splays and fault bounded panels. In general, the SWFZ is the core of an anastomosing network of faults and shear zones of variable dimensions and orientations.

2.3 Meston Lake Property Geology

Sparse outcrop in the Meston Lake property area indicates the area is primarily underlain by diorite to gabbro and variably foliated granodiorite (Figure 4). Foliation within the granodiorite strikes east-west, dips vertically, and is most intense within the Meston Lake Showing area and near the contact with diorite to gabbro intrusions.

2.4 Quaternary Geology

Although Northwestern Ontario was covered by several ice sheets throughout the Pleistocene, almost all of the features in the present day landscape were formed during the late Wisconsin glaciation. During this period, ice flow was directed from two lobes of the Keewatin Ice Divide centred in Nunavut which consisted of an older eastern lobe, and a younger western lobe separated by the Sachigo interlobate moraine which forms a prominent north-trending topographic feature in the present day landscape east of Stull Lake (Figure 5).

East of the Sachigo interlobate moraine, the predominant direction of glacial striae is southwesterly. Drumlins and drumlinoid ridges between Whithers Lake and Misikeyask Lake and in the Muskrat Dam area commonly trend between 220oand 230°, parallel to the glacial striae. Both Tyrrell (1913) and Hudec (1964) mapped striae near Big Trout Lake that indicate an earlier direction of ice movement from southeast to northwest. Similarly trending striae are also found near Muskrat Dam Lake, but the direction of ice movement could not be determined (Ayres, 1966).

Eskers which form relatively continuous ridges of sand and gravel throughout the Meston Lake area are generally less than 15 m high. The distribution of eskers is in the region is shown in Figure 5. The convergence of several eskers indicates that the subglacial streams generally flowed toward the southwest. The general lack of eskers


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west of Sakwaso Lake and south of the Opasquia end moraine reflects the destruction of eskers by wave action in a post glacial lake.

Thick deposits of varved clay and wave modified eskers in the Meston Lake area indicate a relatively long-lived glacial lake occupied the region during the final retreat of the Laurentide ice sheet during the Wisconsinan. Ayres (1966) located the eastern edge of a major glacial lake near the Windigo River, and notes that the elevation of beach deposits on the Opasquia and Sachigo moraines infer that the lake must have been at least 60 m deep during one of its stages. Satterly (1937, 1938) mapped varved clays on either side of the Sachigo interlobate moraine and was able to show by correlation that contemporaneous glacial lakes, which he named Glacial Lakes Ponask and Sachigo, existed on either side of the moraine. Varved clay deposits on Kistigan and Rourke lakes indicate these pro-glacial lakes likely extended as far north as the Ontario-Manitoba boundary, whereas Elson (1967) concluded that Glacial Lake Sachigo may have been separated from the main body of Lake Agassiz when the water level dropped below the elevation of the divide at the west end of the Cobham River watershed. Following the breakup of the Laurentide ice sheet in Hudson Bay, ca. 7500-8000 yrs BP, the northern end of Glacial Lake Sachigo was opened and the lake drained in a series of stages through the Echoing and Sachigo rivers north into Hudson Bay.

3.0 ECONOMIC GEOLOGY

Past exploration in northeastern Ontario and northwestern Manitoba has discovered gold mineralization at several locations along the Stuii-Wunnumin Fault, most notably in the Stull Lake, Rowlandson Lake and God's Lake areas, as well as in splays and regional subparallel faults of the Stuii-Wunnumin Fault Zone which include the North CaribouTatogan Lake Fault in Ontario (Musselwhite gold mine); the Savage Island shear zone at Island Lake, Manitoba (High Rock Island and Island Lake gold mines); as well as the Lingman Lake shear zone (Lingman Lake gold mine) and the South Kenyon fault (Sachigo River gold mine) in Manitoba.

Because of its relatively remote location and intermittent bedrock exposures, the StuiiWunnumin Fault has received very little prospecting and exploration compared to similar sized structures in the Abitibi belt where gold was discovered in 1907, and production has been continuous since 1910.

The Sachigo River Mine in the adjacent Ellard Lake Greenstone Belt represents the only past producing mine in the greater Meston Lake area, having produced 1 ,635 kg of gold at an average grade of 38 g/t Au from a narrow, high-grade vein between 1938 and 1941. During its lifetime the Sachigo River Mine was the highest grade gold producer in Canada (Stone eta/., 2000b). The current ownership and exploration status of the mine property is unclear.

The Sachigo River deposit is hosted by mafic metavolcanic rocks cut by diorite and porphyry dykes. The No. 2 vein, located north of Foster Lake comprises a series of quartz-sulphide veins localized along the contact of a quartz-feldspar porphyry. Overall the zone strikes west (280°) and dips steeply north with an average width of 0.9 m. Mineralization in the No. 2 vein has been traced by drilling for 160 metres along strike to a depth of 300 metres. High grade gold mineralization {>1 opt Au) occurs in blue-grey to glassy quartz veins containing pyrite, pyrrhotite, galena, chalcopyrite and native gold. Lower grade gold mineralization (0.51 to 1.0 opt Au) is associated with grey-white quartz


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lenses hosting pyrite, pyrrhotite, galena and chalcopyrite across widths up to 2.1 m (Valliant, 1980).

4.0 PREVIOUS INVESTIGATIONS

Mineralization in the vicinity of the Meston Lake property includes the Meston Showing, a Mo-Au showing located in the Withers Lake Area (Stone eta/., 2000a, Map P3419). The showing is located on ground which was subsequently staked by Luc Landry. Ontario Geological Survey Map P3419 also identi"fies several drillhole collars targeting metasedimentary sequences south of Meston Lake. The results of the drilling are not indicated in any government assessment file data however.

The Meston Showing consists of a narrow (10 em wide) zone of molybdenum contained within a broader interval of widely spaced quartz veinlets and variably silicified granodiorite that is exposed in several outcrops across a 350 x 130 m area. In 2002, Aurora Platinum acquired one claim (208 ha) immediately east of the Meston Showing and completed reconnaissance geological mapping, prospecting (7 samples) and helicopter supported till and heavy mineral sampling (14 samples) in the area.

The prospecting and sampling indicated quartz-sulphide veining in the showing area was characterized by elevated Au and Cu values and by locally elevated Mo concentrations. Grab samples of gabbro and diorite outside the showing were seen to contain low Cu, Ni and Pt values. The ground was subsequently allowed to lapse.

5.0 INVESTIGATIONS

Investigations undertaken during the reporting period are summarized as follows:

Table 2: Table of Investigations- 2010 Meston Lake Exploration.

Mapping:

Air Support: Forest Helicopters Inc. Kenora, Ontario:

Analysis and Assaying: Saskatchewan Research Council Saskatoon, Saskatchewan:

5.1 Geological Mapping

1 manday

Eurocopter AS 350BA: 1.9 hours

4 samples

Owing to the lack of large lakes which might accommodate fixed-wing aircraft, the evaluation of the Meston Lake property was undertaken during September 2010 using a Eurocopter A-Star helicopter landing on temporary sites in swamps or in burned over areas on the property.


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5.2 Fire Assay

Four grab samples collected during the evaluation of the Meston Lake property were submitted to the Saskatchewan Research Council Geoanalytical Laboratory (SRC) located in Saskatoon, Saskatchewan for gold determination by fire assay and multi-element ICP analysis. A description of the samples is shown in Appendix 1 (Sample Descriptions). The assay lab certificates of analysis are shown in Appendix 2.

Upon receipt at the SRC's facilities, samples are placed in a drying oven if necessary until dry. The entire sample is then crushed to approximately -10 mesh using a jaw crusher. A 500 g sample is then split off from the sample using a Jones riffle splitter. Sub-samples are then pulverized to 90% -15 mesh (105 microns) using a TM Engineering ring and puck pulverizer with 1 kg bowls. The bowls were cleaned with silica sand substitute between each sample to prevent cross-over contamination from one sample to the next. A one assay tonne fire assay is then undertaken on a representative 30 gram sample split from the -105 mesh fraction.

For flame AAS determination of gold, a preliminary concentration by fire assay was used by the SRC which consisted of a series of controlled steps involving weighing, fluxing, fusion and cupellation.

The basic procedure for fire assay involves mixing a 30 g aliquot of pulverized sample material with C02 (soda ash), borax, PbO, flour, nitrate and silica. To this mixture, Ag or Pd is added in solution as a collector. After mixing, the material is fired at a temperature of 1 ooooc for 1% hours. Upon firing, the Pb and Ag in the melt settle to the bottom of the crucible, scavenging gold from the melt. The hot molten mixture is then poured into a mould and upon cooling, the slag separates cleanly from the lead button which should be a certain weight. The button is then placed into a pretreated cupel with the lead absorbed by the cupel leaving a bead which has collected gold as well other platinum group elements. After the lead buttons are cupelled at 1 ooooc for 50 minutes, the gold is then separated from the collector by total dissolution using a nitric/hydrochloric acid digestion bulked up by a 1% La20 3-distilled water solution. The final determination for gold is then made using a Varian AA240 model atomic absorption spectrometer (AAS).

As an International Standards Organization (ISO 17001) and Canmet accredited facility, the Saskatchewan Research Councils laboratory reports are produced using LIMS information management system which indicate all duplicate assays, internal control standards and blanks on the lab's certificate of analysis (Appendix 2). For each quality control standard, control charts are produced to monitor the performance of the laboratory. Warning lines on the chart are set at ±2 standard deviations, and control lines are set at ±3 standard deviations. Any data that falls between ±2 and ±3 standard deviations requires 10% of the samples in that particular batch to be reassayed and have their values compared with the results of previous data sets. Results will be accepted as long as the standards for each batch of samples fall below the standard deviation lines. Any data that falls outside the ±3 standard deviation lines will result in rejection of all the results and reassay of the entire batch of samples .

5.3 Multi-Element ICP Analysis

Since most economic gold deposits in the Superior Province are characterized by relatively wide envelopes of intense hydrothermal alteration, a suite of ICP-MS analyses


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(inductively coupled plasma mass spectroscopy) was undertaken on each of four samples collected during the Meston Lake evaluation in order to quantify the tenor of various pathfinder elements associated with gold mineralization in the region. The tabulated results of the ICP analyses are shown in Appendix 2.

ICP-MS is a widely accepted technique for the measurement of many trace elements to extremely low detection limits. The Saskatchewan Research Council was contracted to perform the analyses on sample pulps which it had analyzed earlier for gold.

The ICP technique involves stripping loosely bound electrons from each element in a sample by means of a high temperature inductively coupled plasma. The resulting ions are then separated on the basis of their mass-to-charge ratio and a mass spectrometer receives a signal proportional to the ion concentration which is calibrated against a series of elemental standards.

ICP analysis requires a sample to be in solution. Initially, samples are pre-screened by ICP-AES to ensure that no elevated metal concentrations (defined as >1% of an individual base metal, or >3% cumulative metal content) are present in order to avoid cross contamination at a later stage during the mass spectrometer reading. Once routine quality control testing has confirmed that samples have met or exceeded specifications, the analytical procedure involves the dissolution of a 0.25 g aliquot of each sample in a hot perchloric-nitric-hydrofloric-hydrochloric digestion. This four acid digestion is among the most powerful acid dissolution procedures used, and all elements for determination are considered to be near total by this method. Following this analysis, the results are reviewed for high concentrations of bismuth, mercury, molybdenum, silver and tungsten and diluted accordingly. Samples meeting this criterion are then analyzed by a suite of 35 elements by ICP-MS.

6.0 RESULTS

6.1 Geological Mapping - Meston Lake Property

Sparse outcrop on the Meston Lake property in conjunction with existing airborne magnetic data indicate the area is primarily underlain by an intrusive suite of diorite to gabbro and variably foliated megacrystic granite, granodiorite and rare tonalite. Foliation within the granodiorite strikes east-west, dips vertically, and is most strongly developed within the Meston Lake Showing area and in areas adjacent to the contact with diorite and gabbro intrusions.

Map 1 further indicates the location of rocks and samples collected during the property evaluation. Appendix 1 provides field notes for each location indicated in Map 1.

Intrusive rocks on the Meston Lake property are interpreted to be younger than the host volcanic strata exposed southeast of Meston Lake and northeast of Blackbear Lake. In regional airborne magnetic surveys, the volcanics are seen to form a subparallel series of sinuous volcanic and sedimentary rocks within the Black Bear Greenstone Belt. Mapping undertaken during the period (Map 1) further indicates the Stuii-Wunnumin Fault which demarcates the southern contact of the Meston Lake property is characterized by numerous high strain zones, typified by the development of schistose


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and gneissic fabrics. Foliations within exposed portions of the Stuii-Wunnumin Fault on the property strike north to northwest with subvertical dips. Local changes in the orientation of the foliation are likely the result of deflection around more competent intrusions.

The metamorphic grade within the belt is middle amphibolite facies based on the assemblage of amphibolite-garnet. Adjacent to the SWFZ a retrograde assemblage of chlorite+feldspar+quartz+carbonate is seen to be developed.

6.2 Prospecting - Meston Lake Property

Mineralization in the Meston Lake property area includes the Meston Lake Showing, a Mo-Au showing located on the Withers Lake mapsheet (OGS map P3419), approximately seven kilometres south of Meston Lake. Re-sampling of a silicified and potassic (biotite) altered, sheared interval of granodiorite hosting trace quantities of fine grained pyrite in the vicinity of the showing (sample R-201 03) returned background gold levels (17 ppb Au, Appendix 2). Three additional samples of sheared diorite and granodiorite elsewhere on the property (samples R-20101, 20102, 20104) returned similarly low gold values (28, 10 and 5 ppb Au , respectively) . ICP analyses of the samples failed to identify any trace element pathfinders normally associated with hydrothermal gold deposits, save for elevated CaO content in one sample (R-201 02: 2.18 wt% CaO- mean of data set: 1.47% CaO, Appendix 2).

Table 3 provides a basic statistical summary for the ICP and gold analyses undertaken on the Meston Lake samples.

Table 3: Statistical Summary of ICP and Gold Analyses - Meston Lake Samples.

Element n Min

Au 4 5

Ag 4 0.1

AI203 4 0.50 As 4 1

Ba 4 53 Be 4 0.5 Bi 4 0.5

CaO 4 0.23

Cd 4 0.5

Co 4 1 Cr 4 76 Cu 4 3

Fe203 4 0.41

Hg 4 0.5

K20 4 0.16

La 4 6

MgO 4 0.1

MnO 4 0.011

Mo 4 2

Northem Superior Resources Inc. Evaluation of the Meston Lake Property

Max Range

28 23

0.1 0

1.2 0.7

2 1

110 57

1.0 0.5

1.0 0.5

2.18 1.95

0.5 0

3 2

96 20

53 50

1.30 0.89

0.5 0 0.28 0.12

57 51

0.6 0.5

0.023 0.012

7 5

8

Mean StdDev Mean+ Median 2&-15 10 35 13.5

0.1 0 0.1 0.1

0.71 0.32 1.35 0.6 2 1 3 2

75 25 126 69

0.6 0.3 1.12 0.5

0.6 0.3 1.12 0.5

0.86 0.91 2.69 0.50 0.5 0 0.5 0.5

1.5 1.2 3.9 1.25

83.8 9.0 101.8 82

22 23 68 15

0.82 0.45 1.72 0.78

0.5 0 0.5 0.5 0.23 0.05 0.33 0.24

23 23.1 69.1 15

0.26 0.24 0.74 0.16

0.019 0.005 0.029 0.020

3.3 2.5 8.3 2

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Na20 4 0.06 0.07 0.01 0.06 0.01 0.07 0.06 Ni 4 3 7 4 4 2 8 3

P20s 4 0.041 0.059 0.018 0.050 0.010 0.070 0.050 Pb 4 2 6 4 3.8 1.7 7.2 3.5 s 4 0.5 0.5 0 0.5 0 0.5 0.5 Sb 4 0.5 0.5 0 0.5 0 0.5 0.5 Sc 4 0.5 0.5 0 0.5 0 0.5 0.5 Se 4 0.5 0.5 0 0.5 0 0.5 0.5 Sn 4 0.5 0.5 0 0.5 0 0.5 0.5 Sr 4 2 83 81 33 35 103 24

Ti02 4 0.02 0.09 0.07 0.05 0.04 0.12 0.03 u 4 0.5 6 5.5 2 2.7 7.4 0.8 v 4 1 7 6 3 2.7 8.4 2.0 w 4 0.5 1 0.5 0.8 0.3 1.3 0.8 y 4 2 108 106 29 53 135 2

Zn 4 11 29 18 18 8 35 17 Zr 4 4 50 46 5.9 10.7 27.3 9

7.0 CONCULSIONS AND RECOMMENDATIONS

The significance of major crustal breaks as first order controls on Archean gold mineralization is well documented (e.g. Bursnall, 1989). In the Abitibi Greenstone Belt of northeastern Ontario and Quebec, gold deposits occur in two distinct linear trends which broadly coincide with the Kirkland Lake/Larder Lake/Cadillac and Destor-Porcupine Faults (Figure 6). These "structural breaks" control the distribution of gold camps at a regional scale that host world-class gold deposits such as the Hollinger-Mclntyre (31.4 M oz Au) and Kirkland Lake (21.4 M oz Au) mines, the 15th and 21st largest gold deposits in the world (Sillitoe, 2000). Within the Abitibi Greenstone Belt, gold deposits are irregularly distributed in clusters along the main breaks, in a diverse number of host rocks and geological settings. Deposits may be located in either proximal or distal settings with respect to the main break, but are always found on secondary or tertiary splays, not the main fault (Valliant and Hutchinson, 1982). For example, in the Porcupine camp, the Dome and nearby deposits are located on secondary splays 400-1,400 metres from the Destor-Porcupine Fault, whereas the Mclntyre-Hollinger Mine and associated deposits are located about 5 kilometres off the main break on subparallel faults. The majority of gold deposits in all of the Abitibi camps occur within a 5 kilometre buffer on either side of the main fault.

A comparison of the size of regional structures in these prolific gold camps versus the Stuii-Wunnumin Fault which bounds the southern margin of the Meston Lake property, indicates, the SWF is almost twice the length of the Abitibi "breaks". Although known gold resources developed to date along the Stull Wunnumin Fault are trivial in comparison to the Abitibi and Red Lake camps, this may be due to historical and geographical rather than geological factors. The primary differences affecting the rate of discovery in the two regions is the relative remoteness of this portion of northwestern Ontario, and consequently, the significantly lower level of historical prospecting and exploration activity. Given the high potential for the discovery of world-class gold deposits along regional faults in Archean terranes, the challenge is to identify


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prospective geological settings where this potential is enhanced in the Meston Lake area.

7.1 Recommendations

Given the sparse occurrence of outcrop across Northern Superior Resource's claims in the Meston Lake area, further exploration will by necessity have to rely upon geophysics, geochemistry, and geological interpretation.

Taking advantage of recent advances in relatively low cost, high resolution airborne survey data, a time domain electromagnetic survey combined with a high sensitivity magnetometer survey is recommended to be completed on the property. The main purpose of the surveys will be: to acquire information with respect to the litho-structural framework on the basis of bedrock magnetic responses, and to identify potential areas of precious and base metal mineralization on the basis of bedrock conductive and magnetic responses.

Among some of the considerations for the proposed airborne survey are: northeast/southwest directed flight lines oriented perpendicular to the trend of the regional geological fabric imposed by the Stuii-Wunnumin Fault, and a 125-150 m survey line spacing with an EM bird terrain clearance of approximately 30 metres.

From the survey data, EIVI anomalies can be evaluated and graded according to the interpreted conductance (conductivity-thickness) based on a vertical thin sheet model response to a mid-frequency coaxial coil configuration. Thereafter, it is recommended that multi-element soil geochemistry survey accompanied by prospecting, sampling and geological mapping be undertaken in area characterized by EM anomalies. The Stull Wunnumin Fault which runs subparallel to the southern margin of the Meston Lake claims presents a strong candidate for additional follow-up investigations.

8.0 PERSONNEL

A total of 15 mandays of work by various contractors was required during the evaluation of Meston Lake property during September 2010. A detailed manday distribution by activity for the period is listed in Appendix 3.

9.0 EXPENDITURES

Allowable assessment expenditures as outlined in the Provincial Mining Act 6/96 for the Meston Lake work program are summarized in Table 4.

Table 4: Exploration Expenditures - 2010 Meston Lake Work Program.

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Food $889.06

Lodging $3,870.63

Salaries $3,657.80

Transportation $11,725.54

Supplies-Equipment Rental $2,404.60


10

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Analyses $167.70

Total= $22,547.63

10.0 REFERENCES

Ayres, L.D., 1966: Geology of the Muskrat Dam Lake Area, District of Kenora (Patricia Portion), Ontario Department of Mines Open File Report 5002, 102 p.

Bennett, G. and Riley, R.A., 1969: Operation Lingman Lake, Ontario Department of Mines IVIiscellaneous Paper 27, 58 p.

Bursnall, J.T., ed. 1989: Mineralization and Shear Zones, GAC/MAC Short Course Notes, Vol. 6, 229 p.

Davis, D.W. and Stott, G.M., 2001: Geochronology of Several Greenstone Belts in the Sachigo Subprovince, Northwestern Ontario, Ontario Geological Survey Summary of Field Work and Other Activities 2001, pp. 18-1-18-13.

Elson, J. A., 1967: Geology of Glacial Lake Agassiz. in W.J. Mayer-Oakes (ed.) Life, Land and Water, University of Manitoba Press, Winnipeg, pp. 36-95.

Hodgson, C. J. and Hamilton, J.V. 1988: Gold Mineralization in the Abitibi Greenstone Belt: End Result of Archaean Collisional Tectonics? in RD. Keays, W.R.H. Ramsay and D.l. Groves, eds. The Geology of Gold Deposits: The Perspective in 1988. Economic Geology Monograph 6, pp.86-100.

Hudec, P.P., 1964: Geology of the Big Trout Lake Area, District of Kenora (Patricia Portion). Ontario Department of IVIines Geological Report No. 23 and Map 2045, 1 :126,720 scale.

Meen, V.B., 1937: Geology of the Sachigo River Area. Ontario Department of Mines Annual Report, Vol. 46, part IV, pp. 32-59.

Osmani, I.A., Stott, G.IVI., Sanborn-Barrie, M. and Williams, H.R., 1989: Recognition of Regional Shear Zones in the South-Central and Northwestern Superior Province of Ontario and Their Economic Significance in J.T. Bursnall (ed.) Mineralization and Shear Zones, GAC/MAC Short Course Notes, Vol. 6, pp. 199-217.

Satterly, B., 1937: Geology of the Stull Lake Area, 46th Annual Report of the Ontario Department of Mines, Map 46C, Part IV, pp. 1-31.

Satterly, B., 1938: Geology of the Sandy Lake Area, 47th Annual Report of the Ontario Department of Mines, Vol. 47 Part VII.


11

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J J ~j

J

Sillitoe, R.H., 2000: Enigmatic Origin of Giant Gold Deposits, in Geology and Ore Deposits 2000: The Great Basin and Beyond, Geological Society of Nevada Symposium Proceedings pp. 1-18.

Skulski, T., Corkery, M.T., Stone, D., Whalen, J.B. and Stern, R.A. 2000: Geological and Geochronological Investigations in the Stull Lake - Edmund Lake Greenstone Belt and Granitoid Rocks of the Northwestern Superior Province in Report of Activities 2000, Manitoba Industry, Trade and Mines, Manitoba Geological Survey, pp. 117-128.

Stone, D., 2001: A Study of Indicator Minerals for Kimberlite, Base Metals and Gold: Northern Superior Province of Ontario; Ontario Geological Survey, Open File Report 6066, 140 p.

Stone, D., Halle, J. and Lange, M., 2000a: Precambrian Geology, Whithers Lake Area; Ontario Geological Survey Preliminary Map P3419, 1:50,000 scale.

Stone, D., Halle, J. and Lange, M., 2000b: The Distribution of Gold Grains in Till, Sachigo River Mine, Northwest Ontario, Ontario Geological Survey Open File Report 6015, 17 p.

Stone, D., Halle, J. and Pufhal, P., 2001: Precambrian Geology, Rapson Bay Area; Ontario Geological Survey Preliminary Map P3451, 1:50,000 scale.

Stott, G.M., 1990: A Classification of Fault Systems and Shear Zones in the Superior Province in F. Robert et a/. (eds.) Greenstone Gold and Crustal Evolution. NUNA Conference Volume, pp. 211-213.

Tyrell, J.B., 1913: The Patrician Glacier South of Hudson Bay, XII International Geological Congress, 1913, Ottawa, Compte Rendu, pp. 523-534.

Valliant, R.I. and Hutchinson, R.W., 1982: Stratigraphic Distribution and Genesis of Gold Deposits, Bousquet Region, Northwestern Ontario in Geology of Canadian Gold Deposits, Proceedings of the CIM Gold Symposium, Sept. 1980. CIM Special Volume 24. pp. 27-40.

Internal Reports

Bradford, J. 2001: Geology of the Wunnumin Lake - Winisk River - Peeagwon River Area, Northwestern Ontario (NTS 53A/9, 10, 14, 15, 16), internal report for Aurora Platinum Corporation.

Bradford, J., 2002: Gold Exploration Targets, Stuii-Wunnumin Fault, Northwestern Ontario and Manitoba, internal report for Aurora Platinum Corporation and Southwest Resources Corporation, March 6, 2002, 29 p.


12

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]

]

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J

]

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Kaip, A. and Childe, F., 2002: AEM Gold Project, Northwestern Ontario/Northeastern Manitoba, Canada, 2002 Exploration Program Summary, internal report for Aurora Platinum Corp., December 16, 2002, 117 p.

Valliant, R.I., 1980: 1980: Sachigo River Project, Report on Geology, internal report for Long Lac Mineral Exploration Ltd., 5 p.


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11.0 STATEMENT OF QUALIFICATIONS

I, Ronald William Avery, P. Geo., as author of the report, titled "Evaluation of the Meston Lake Property, NTS 53 J/4, Meston Lake, Red Lake Mining District, Ontario", prepared for Northern Superior Resources Inc. and dated January 2011, do hereby certify that:

1. I am a consulting geologist employed by Greenstone Geological Consulting Ltd. located at 103-2730 Main Street, Saskatoon, Saskatchewan, Canada.

2. I am a member in good standing of the Association of Professional Engineers and Geoscientists of Saskatchewan (member number 9782) . I am a registered Professional Geologist with APEGS with additional Permission to Consult.

3. I am a graduate of Queen's University at Kingston, Ontario with combined B.Sc. Honours degrees in Physical Geography (1987) and Geology (1988).

4. I have practiced my profession continuously since graduation in 1988, and have been involved in mineral exploration throughout Canada, the United States, Myanmar, Indonesia and the Philippines.

5. I am independent of the issuer applying the test set out in section 1.4 of National Instrument 43-101.

6. The foregoing report is based on:

• my personal knowledge of the geology of the property gained through study of historical exploration data and current property data supplied to me by Northern Superior Resources Inc.

• a site visit to the Meston Lake property on September 11 , 201 0 in order to assess the geology and previous exploration undertaken on Northern Superior's property.

7. I am not aware of any material fact or material change with respect to the subject matter of this technical report which is not reflected in this report, the omission to disclose which would make this report misleading.

Dated at Saskatoon, Saskatchewan, this 281h day of January, 2011 .

l(q!fi1 SIGNED "R.W Avery" (signed and sealed)

R.W. Avery, B.A. , B.Sc., P. Geo Greenstone Geological Consulting Ltd.


14

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Appendix 1: Meston Lake Sample Descriptions


Property Station Statn_typ Statn desc SampNum LabNum LatGPS84 LongGPS84 UTM Datum UTM Zone UTMEast83 UTMNorth83 GPS_Eiev_m DateThile SampType Width m sam rocknm Meston 001 swamp NAD83 15U 579621 6014024 11-Sep-10

Meston 002 outcrop 20101 G-2010-1446 NAD83 1SU 578014 6013393 . 11-Sep-10 grab sheared diorite

1 Meston 003 outcrop NAD83 15U 582646 6010898 11-Sep-10 .

Meston 004 outcrop NAD83 15U 582583 6010886 11-Sep-10

Meston 005 outcrop 20102 G-2010-1446 NAD83 15U 582611 6010870 11-Sep-10 grab sheared granodiorite

Meston 006 till NAD83 15U 582673 6011100 11-Sep-10







Meston 013 outcrop NAD83 15U 580498 6010427 11-Sep-10 ..



Meston 016 outcrop 20103 G-201 0-1446 NAD83 15U 581920 6012221 11-Sep-10 grab



Meston 019 outcrop NAD83 . 15U 581768 6012271 11-Sep-10


Meston 021 till NAD83 lSU 581507 6012154 11-Sep-10

Meston 022 till NAD 83 15U 581565 6012160 11-Sep-10


Meston 024 outcrop NAD83 1SU 581705 6012216 11-Sep-10






Meston 030 outcrop NAD 83. 15U 580182 6013582 11-Sep-10

Mestori 031 outcrop NAD83 15U 580156 6013618 11-Sep-10

Meston 032 outcrop NAD83 lSU 580152 6013678 11-Sep-10 ,

Meston 033 outcrop NAD83 lSU 580127 6013692 11-Sep-10





Meston 038 outcrop NAD83 15U 582436 6011117 11-Sep:lO

Meston 039 outcrop 20104 G-2010-1446 NAD83 1SU 582433 6011124 11-Sep-10 grab



Northern Superior Resources ln.

Meston Lake Property Evaluation- September 2010 1

001

002

003004

005006007

008009

010

011012013

014015

016

017

018019020021022023024025

026

027028029030031

032

033034035

036037

038

039

040041

Station

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Appendix 2: Certificates of Analysis -Saskatchewan Research Council


0

0

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u 0 D

smart science solutions

Saskatchewan

Research Council

125 -151nnovation Boulevard, Saskatoon, SK Canada 57N 2X8 • Ph: 306-933-5400 Fax: 306-933-7446 Also located at: 129 -6 Research Drive, Regina. SK Canada 545 7J7 Ph : 306-787-9100 Fax: 306-787-88'11 Also lowed at. 101· 1061 Centr<ll Ave., Prince Albert, SK Canada S6V 4V~ • Ph: lOii-765-2340 F,H: 306-765-234-1

Web: www.src.sk.ca

Email: [email protected]

Report No: G-1 0-1446

SRC Geoanalytical Laboratories

Northern Superior Resources 1988 Kingsway,Unit G Sudbury, Ontario P3B 4J8

Attn: Ron A very

125- 15 Innovation Blvd. Saskatoon, Saskatchewan

S7N 2X8

Phone: (306) 933-8118 Fax: (306) 933-5656

January 27, 2011

Test reports are the property of the customers. Publications of statements, conclusions or extracts from these reports are not permitted without prior written permission from the customer.

This document constitutes the final official test report. Liability for the SRC Geoanalytical Laboratories', if any, will be limited to the cost of analysis for samples in this test report. The results contained in this test report relate only to the items tested. It is the customer's responsibility to ensure that all interpretation of analysis is done using the data from this report.

The customer will not use the name of the Saskatchewan Research Council in connection with the sale, offer, advertisement or the promotion of any article, product, or company without the prior written consent ofthe SRC.

~~

Results Reviewed and Approved by: ---t~'----v'--'~'="'=- .<-·' _ -__ _,d._. --'~'-----" ...... )ti<-~"""'=-2:""": ::..>..------

Robert Millar Assistant Research Scientist

[____

Northern Superior Resources Attention: Ron Ave!) PO #/Project: Samples: 25

Column Header Details

Silver in ppm (Ag) Aluminum in wt % (AI203) Arsenic in ppm (As) Barium in ppm (Ba) Berylium in ppm (Be)

Bismuth in ppm (Bi) Calcium in wt % (GaO) Cadmium in ppm (Cd) Cobalt in ppm (Co) Chromium in ppm (Cr)

Copper in ppm (Cu) Iron in wt% (Fe203) Mercury in ppm (Hg) Potassium in wt % (K20) Lanthanum in ppm (La)

Magnesium in wt% (MgO) Manganese in wt % (MnO) Molybdenum in ppm (Mo) Sodium in wt% (Na20) Nickel in ppm (Ni)

Phosphorus in wt % (P205) Lead in ppm (Pb) Sulfur in ppm (S) Antimony in ppm (Sb) Scandium in ppm (Sc)

Selenium in ppm (Se) Tin in ppm (Sn) Strontium in ppm (Sr) Titanium in wt % (Ti02) Uranium in ppm (U, ICP)

Vanadium in ppm (V) Tungsten in ppm (W) Yttrium in ppm (Y) Zinc in ppm (Zn) Zirconium in ppm (Zr)

~ l__J [___J ~ ~ SRC Geoanalytical Laboratories

125- 15 Innovation Blvd., Saskatoon, Saskatchewan, S7N 2X8

Tel: (306) 933-8118 Fax: (306) 933-5656 Email: [email protected]

Multi-Element ICP Analysis Aqua Regia Digestion

Report No: G-1 0-1446

Date of Report: January 27,2011

Page 1 of 3 This data has been approved for release by: &- J1t.4 Date: 01/27/2011

' L-.: I ~ ' 1 L.__j L_j r ~ '1

~ :____j L_j ~ L_ ~ ~ L_ ·~

L______; :_________; '---- i...._____j ---..!

SRC Geoanalytical Laboratories Report No: G-10-1446 Northern Superior Resources 125- 15 Innovation Blvd., Saskatoon, Saskatchewan, S7N 2X8 Attention: Ron A vet) Tel: (306) 933-8118 Fax: (306) 933-5656 Email: [email protected] PO #/Project:

Date of Report: January 27,2011 Samples: 25 Multi-Element ICP Analysis

Aqua Regia Digestion

Sample Ag Al203 As Ba Be Bi CaO Cd Co Cr Cu Fe203 Hg K20 La MgO MnO Mo Number ppm wt% ppm ppm ppm ppm wt% ppm ppm ppm ppm wt% ppm wt% ppm wt% wt% ppm

LS4 <0.2 5.62 12 303 2.0 <1 0.48 39 87 49 10.3 <1 0.47 39 1.08 0.647 15 20101 <0.2 0.55 2 78 1.0 1 0.23 <1 <1 96 25 1.30 <1 0.25 57 0.16 0.011 7 20102 <0.2 0.59 1 110 <0.5 <1 2.18 <1 2 78 5 0.41 <1 0.23 16 0.16 0.020 2 20103 <0.2 1.19 2 53 <0.5 <1 0.76 <1 3 85 53 1.10 <1 0.28 6 0.62 0.020 2 20104 <0.2 0.51 1 60 <0.5 <1 0.26 <1 <1 76 3 0.45 <1 0.16 13 0.11 0.023 2

Page 2 of 3 This data has been approved for release by: Date: 01/27/2011

L__ 1 c r , ' '1

'----' '-----..! '- '-------' ---- '-----' L__j L___j '--- '-------.; '--------' .____; _ _j ~

SRC Geoanalytical Laboratories Report No: G-10-1446

Northern Superior Resources 125 - 15 Innovation Blvd., Saskatoon, Saskatchewan, S7N 2X8 Attention: Ron A vel) Tel: (306) 933-8118 Fax: (306) 933-5656 Email: [email protected] PO #/Project:

Date of Report: January 27, 2011 Samples: 25

Multi-Element ICP Analysis Aqua Regia Digestion

Sample Na20 Ni P205 Pb s Sb Sc Se Sn Sr Ti02 U, ICP v w y Zn Zr Number wt% ppm wt% ppm ppm ppm ppm ppm ppm ppm wt% ppm ppm ppm ppm ppm ppm

LS4 0.02 48 0.569 27 1770 <1 7 <1 <1 22 0.16 34 101 <1 18 209 <1 20101 0.06 3 0.041 4 1930 <1 <1 <1 <1 2 0.03 6 2 1 108 13 50 20102 0.06 3 0.058 6 344 <1 <1 <1 <1 83 0.02 <1 2 <1 2 20 9 20103 0.07 7" 0.059 3 610 <1 <1 <1 <1 21 0.09 <1 7 1 2 29 4 20104 0.06 3 0.042 2 14 <1 <1 <1 <1 26 <0.01 1 1 <1 2 11 8

Page 3 of 3 This data has been approved for release by: ~-· /('d1 Date: 01/27/2011

Northern Superior Resources Attention: Ron A vel) PO #/Project: Samples: 25

Column Header Details

Au Fire Assay by ICP in ppb (Au)

Sample Number

LS4 20101 20102 20103 20104

Au ppb

N/R 28 10 17

5

L_j l_j [__J L.____; SRC Geoanalytical Laboratories

125- 15 Innovation Blvd., Saskatoon, Saskatchewan, S7N 2X8

Tel: (306) 933-8118 Fax: ·(306) 933-5656 Email: [email protected]

Fire Assay

Report No: G-10-1446

Date of Report: January 27,2011

Fire Assay: A pulp is subjected to standard fire assaying procedures.

Page 1 of 1 This data has been approved for release by: ----P-il~V---.~/z...--'--M""L""~:..::· :..t...l_ Date: 01/27/2011

0 D D

0

0 0 0 0

D

0 D

0 0 0 D

u

SRC Sample" Group# Identifier

G-2010-1446 20101

G-2010-1446 20102

G-2010-1446 20103

G-2010-1446 20104

mean std dev

mean + 2 std dev min

max range

variance

sum SumSq median

Sample Standard Data

G-2010-1446

G-201 0-1446

Northern Superior Resouces Inc.

Meston Lake Assay Database

L$4

L$4

Au Ag Al203

ppb ppm 'lit% 28 <0.2 0.55

10 <0.2 0.59

17 <0.2 1.19

5 <0.2 0.51

15 0.1 0.71

10 0.0 0.32

35 0.1 1.35

5 0.1 0.5

28 0.1 1.2

23 0.0 0.7 99.3 0.0 0.1

60 0.4 2.8

1198 0 2.3

13.5 0.1 0.6

<0.2 5.62 <0.2 5.9

As Ba Be Bi CaO Cd ppm ppm ppm ppm wt% ppm

2 78 1 1 0.23 <1

1 110 <1 <1 2.18 <1

2 53 <1 <1 0.76 <1

1 60 <1 <1 0.26 <1

2 75 0.6 0.6 0.86 0.5

1 25 0.3 0.3 0.91 0.0

3 126 1.12 1.12 2.69 0.5 1 53 0.5 0.5 0.2 0.5

2 110 1.0 1.0 2.18 0.5

1 57 0.5 0.5 1.95 0.0

0 648 0.06 0.06 0.84 0

6 301 2.5 2.5 3.4 2.0 10 24593 1.75 1.75 5.5 1.0

2 69 0.5 0.5 0.5 0.5

12 303 2 <1 0.48 1

11 310 2 <1 0.47 1

Co Cr Cu Fe203 Hg K20 La MgO MnO Mo Na20 Ni P205 f.>b I ppm ppm ppm wt% ppm wt% ppm wt% wt% ppm wt% ppm wt% ppm

<1 96 25 1.3 <1 0.25 57 0.16 O.Q11 7 0.06 3 0.041 4

2 78 5 0.41 <1 0.23 16 0.16 0.02 2 0.06 3 0.058 6

3 85 53 1.1 <1 0.28 6 0.62 0.02 2 0.07 7 0.059 3

<1 76 3 0.45 <1 0.16 13 0.11 0.023 2 0.06 3 0.042 2

1.5 83.8 22 0.82 0.5 0.23 23 0.26 0.019 3.3 0.06 4 0.050 3.8

1.2 9.0 23 0.45 0.0 0.05 23.1 0.24 0.005 2.5 0.01 2 0.010 1.7

3.9 101.8 68 1.72 0.50 0.33 69.1 0.74 0.029 8.3 0.07 8 0.070 7.2

1 76 3 0.4 0.5 0.2 6 0.1 0.011 2 0.06 3 0.041 2

3 96 53 1.30 0.5 0.28 57 0.6 0.023 7 0.07 7 0.059 6

2.5 20 50 0.89 0.0 0.12 51 0.5 0.012 5 0.01 4 0.018 4

1.1 82 540 0.2 0.0 0.00 531 0.06 0.000 6 0.000 4 0.000 2.9

6 335 86 3.3 2.0 0.9 92 1.1 0.074 13 0.250 16 0.200 15

13.5 28301 3468 3.3 1.0 0.2 3710 0.4 0.001 61 0.02 76 0.010 65

1.25 82 15 0.78 0.5 0.24 15 0.16 0.020 2 0.06 3 0.050 3.5

39 87 49 10.3 <1 0.47 39 1.08 0.647 15 0.02 48 0.569 27

39 85 53 10.5 <1 0.5 42 1.14 0.657 14 0.02 50 0.569 25

1

0 0 0 0 0 0

D D 0 0 0 D

D 0 u D

D

s ....

Sb ppm ppm 1930 <1 344 <1 610 <1 14 <1

725 0.5 840 0.0 2404 0.50

14 0.5 1930 0.5 1916 0.0

705310 0.0 2898 2.0

4215532 1.0 477 0.5

1770 <1 1800 <1

Northern Superior Resouces Inc.

Meston Lake Assay Database

Sc . ... sn ~ --·~

Se Sr Qj:)m _._R~~ ""-- j:));)rtl l....,..j:)Qm

<1 <1 <1 2 <1 <1 <1 83 <1 <1 <1 21 <1 <1 <1 26

0.5 0.5 0.5 33 0.0 0.0 0.0 35 0.50 0.50 0.5 103 0.5 0.5 0.5 2.0 0.5 0.5 0.5 83.0 0.0 0.0 0.0 81.0 0.0 0.0 0.0 1218 2.0 2.0 2.0 132 1.0 1.0 1.0 8010 0.5 0.5 0.5 24

7 <1 <1 22 7 <1 <1 24

Ti02 u ~· ~

Zn Zr w y

wt% ppm ,_ );));)ill...,. ppm ... ppm ... .. PPm. . .. ppm 0.03 6 2 1 108 13 50 0.02 <1 2 <1 2 20 9 0.09 <1 7 1 2 29 4 <0.01 1 1 <1 2 11 8

0.05 2 3 0.8 29 18 5.9 0.04 2.7 2.7 0.3 53 8 10.7 0.12 7.4 8.4 1.3 135 35 27.3 0.02 0.5 1 0.5 2 11 4 0.09 6 7 1 108 29 50 0.07 5.5 6 0.5 106 18 46 0.00 7.2 7 0.1 2809 66 467 0.14 8 12 3 114 73 71 0.01 37.5 58 2.5 11676 1531 2661 0.03 0.8 2.0 0.8 2 17 9

0.16 34 101 <1 18 209 <1 0.16 36 105 <1 18 217 <1

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Appendix 3: Manday Distribution- 2010 Meston Lake Exploration


L....J [_J LJ

Personnel SEPTEMBER 2010 Northern Superior Resources Inc. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 Total Ron Avery- Consulting Geologist - - - - - - - - - m G - - - - - - d - - - - - - - - - - - - 3

Northern Superior Resources total: 3 Sachigo First .Nation Andy Tardiff- Camp Manager/Cook - - - - - - - - - c c - - - - - - c - - - - - - - - - - - - 3 Isaac Barkman - Field Assistant - - - - - - - - - m F - - - - - - L - - - - - - - - - - - - 3 Willian Oombash- Camp Assistant - - - - - - - - - m ca - - - - - - ca - - - - - - - - - - - - 3

Sachigo First Nation total: 9 Forest Helicopters Ltd. Dale Warketin- Helicopter Pilot - - - - - - - - - m H d - - - - - - - - - - - - - - - - - - 3

Forest Helicopters total: 3

September mandays total: I 15

m: mob; d: demob; L: logistics r: report writing; G: geological mapping; T: trench mapping; H: helicopter support; A: aircraft support; F: field assistant w: weather day; C: cook ca: camp attendant; Cr: community liason

Northern Superior Resources Inc. Meston Property Evaluation - Manday Distribution

[_]

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Figure 3: Tectonostratigraphic Components of the Northwest Superior Province.

1 Q Kil0metres

(Figure adapted from Skulski eta/., 2000)


limestone c.rbarwtle Monr.odlorite, monzonite, granite (sanUdtold Sl.ile)

~ Cofvlomerate, sandltme, alkalne Wkanic rock

~ San:latone, liltatone

<D Biatite granite

<W;> Peraluminous granite

c:::J> Hofrblende tonalite

to granie

C> Bietite tonalite

<([J]D> Tolllllite gneiss c:::> lntennedlate to felsic

metavoiCW!ic rock €J> Mafic to ultramafic

metavoklanic rock ~ GaW>ro, diode

'""" Falit zone

]

J

Figure 5: Surficial Geology of Northwestern Ontario.

D Organic deposit ~ Fluvial deposit [J] Glaciolacustrine deposit

(sand, gravel)

D -Glaciolacustrine deposit (silt, clay)

Glaciofluvial lea-contact deposit

D Till E3 Bedrock ~ Drumnn 0 Esker [2] Trand of and

moraine crest

1.,r' Glacial striae

10

l<ilomeires

Figure 2: Quaternary geology of the northern Superior area.

(Figure adapted from Stone, 2001)


47

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Fjgure 6: Association of Gold Deposits and Regional Faults- Abitibi Greenstone Belt.

Timmins

---Legend

~ Clastic sedimentary rocks: ~ Younger (Timiskaming Gp}/Oider (Porcupine Gp) \ I] Felsic porphyry and related intrusions

_- Main 'breaks'

------ 01 Shear zones .-- 02 Shear zones

/ Axial surface trace of 01 folds 'NW-trending lineament

" . d . A . A Producmg or paS1·pro ucmg u mme • Kidd Creek Cu-Zn deposit

T Timmins camp M Matachewan camp

KL Kirkland Lake camp

(Figure adapted from Hodgson and Hamilton, 1988)


I \ N

• I

\ '-------

-_,,L..----~ Kirkland-Larder Lake Area

0 0 0 ..r 'P' 0 U)

0 0 0

580000

no ole

4250851

581000 582000 583000

N

no ole

584000

Rapson Bay· Meston Lake Mapping Legend 082 Spreadsheet notation, sample description

(;; Claim post

\\\' Area of shoreline traverse 80

\. Fold axis and plunge

8~ Foliation strike and dip

~ Glacial striae

~ Joint strike and dip

~ Quartz vein strike and dip

~~ )'t .. Shearing strike and dip

80 ,. Outcrop

R-20122 Rock sample location

Alteration I Abbreviations

q Quartz vein b, bioi Biotite bx Breccia py Pyrite silic Silicification hem Hematite

~11--------------~~--------t---------------------------------------------------------t-------------------------j---~~~~-----------------------------:-------------------------------L __________ -r--------~--------~~---------r-o IQ

0 0 0 N 'P' 0 U)

··--· -~

·-·-· ~ -~1~.~~-;~:i'' ~ i3:: 1--------

••• :. :~:. " :"'"'' · ::::.. · - ::: •• :·~ :!.:. ··:-·- · · ::::.

--~--------------------·----·---------~~~~~~;~~~--~.~~~~·~--:~~~~~-~~~~rw.8~~~~;~::_~ .. · ·;,~~~~·-~.:J~~: ~-~~~rw.~;~~~;~::.::~· .-.... ·-~---j~~~~~~~~~~~~~~~~==-------·----·---~~-------------------------~ /1 xq

83

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q

:~_/f:ilii·::~2-- -~_·:-.:~_/1~-.w./\-.~: -~-~-~;~:r!':iJI/~;-.~-- ~--~-~-~f.':~::-~~-~-: :~-~-~:~Jt~·:.: · .. ·~ ...... ~ ....... ---~ ....... ~ ....... · .. ~ ....... tto ·oJ~ ....... ~ ....... ,.-~ ·

·~~~~!:~~;;:;:r~·s;; ~;;:([~;~;;'~·, ,_ '=L~ ~--~~r= .:~::·: ,~;,::::~· .... 42 50854

.. ;.; .. ..:-· .....

' I

biot, py, silie, mag

4250853

R-20104 si lie, biot, bx

'* !52

, ole (approxl

no ole >(

0 0 0 ..r 'P' 0 U)

0 0 0 M .... 0 IQ

0 0 0 N 'P' 0 U)

0 0 0 0

~~-----------------4----------~------------------------------------------------------------------+------------------------------+------~~-A~~.-----~~~~~~~--~~~~~~~---------------------------------------------1------------~~~--------~--~----~~

~ :;----""'-'-~-:-,.·:·_:·:_:. . . .• · R-2010~~;!!~i~f:~wifti~~~ i

l_ ____________ _

012 013 './ . ..L--r-1 --,7...-011 80

.,~

80/

58()000 581000

005 py-s11.1c-.he.~ ...... ·-· ..... .. , .. ~ .......... ..... .. , .. ~

----------~~r~~-b~u!~~~-~~~t~~i~~;~:;r· r-------------'--1--------------------------------''------, ~:~-- -~;~=::·~~~~-{:';li/ ·;.:·

1:10,000

0 0.125 0.25 0.5 0.75

Kilometers

582000 583000

Proj

Superior Resources Lake Mapping Project

on: NAD83 Zone 15N

584000

Date post:	06-Jul-2020
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Evaluation of the Meston Lake Property NTS 53 J/4 Meston Lake · which rim of the Superior...

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