TABLE OF CONTENTS
ITEM 1: SUMMARY 4
ITEM 2: INTRODUCTION AND TERMS OF REFERENCE 7
ITEM 3: RELIANCE ON OTHER EXPERTS 7
ITEM 4: PROPERTY DESCRIPTION AND LOCATION 8 4.1 Location 4.2 Property Description 4.3 Provincial Mining Regulations
ITEM 5: ACCESSIBILITY, PHYSIOGRAPHY, INFRASTRUCTURE 10
ITEM 6: HISTORY OF PREVIOUS EXPLORATION 12
ITEM 7: GEOLOGICAL SETTING AND MINERALIZATION 13 7.1 DOK 35 Area 14 7.2 Teck Area 15 7.3 Strata Creek Area 15 7.4 Yeti Area 15 7.5 Yehiniko East Area 16
ITEM 8: DEPOSIT TYPES 8.1 Characteristics of Alkalic and Calc-Alkaline Copper Gold Deposits 16 8.2 Description of the Galore Creek Deposit 8.2 Description of the Schaft Creek Deposit
ITEM 9: EXPLORATION 9.1 Exploration Work Completed in 2012 by Brades Resources 18 9.2 Statement of Costs for SOW No: 5447737, 5453427, 5464789, 5474146, 5474763 ITEM 10: DRILLING 24
ITEM 11: SAMPLE PREPARATION, ANALYSIS AND SECURITY 24
ITEM 12: DATA VERIFICATION 24
ITEM 13: MINERAL PROCESSING AND METALLURGICAL TESTING 25
ITEM 14: MINERAL RESOURCE ESTIMATES 25
ITEM 15 -22: ADVANCED PROPERTY DISCLOSURE 25
ITEM 23: ADJACENT PROPERTIES 25
ITEM 24: OTHER RELEVENT DATA AND INFORMATION 25
Assessment Report dated December 30, 2013 2 ITEM 25 - 26: CONCLUSIONS AND RECOMMENDATIONS 26
ITEM 27: SOURCES OF INFORMATION 27
DATE AND SIGNATURE PAGE Certificate of Qualified Person: C. von Einsiedel, P.Geo. 28
APPENDIX 1 LIST OF REPORT FIGURES
Figure 1: Locator map of NW BC’s Iskut River District showing staked areas, mines and advanced prospects, parks, access roads and local communities (1:2,000,000). Figure 1A: North Iskut River District Area Map Showing Ownership and Porphyry Copper Gold Prospects (1:750,000 scale) Figure 2: Geological map of NW BC’s Iskut River District showing mines and advanced porphyry copper prospects (1:2,000,000). Figure 3: Regional scale geological map showing Galore Creek, Schaft Creek and the BRC Property (1:250,000). Figure 4: Regional scale stream sediment survey map showing copper anomalies associated with Galore Creek, Schaft Creek and the main areas of interest within the BRC Property (1:250,000). Figure 5: Regional scale airborne magnetic survey map showing Galore Creek, Schaft Creek and the BRC Property (1:250,000). Figure 6: BRC Project area map showing mineral claim tenure reference numbers, location of 2013 exploration programs (1:100,000). Figure 7: DOK 35 Area Geological Map and Index Map Showing BC Minfile Prospects and Exploration Work Completed by Brades in 2013 (1:100,000 scale) Figure8: DOC 35 Area Index Map Showing Areas of Historic Sampling by Sample Type and Location of 2013 Soil and Rock samples (1:25,000 scale)
LIST OF LARGE FORMAT TECHNICAL FIGURES TO SHOW 2013 EXPLORATION WORK
Figure LF-01: DOK 35 AREA Detail Map Showing 2013 and Historic Rock, Stream and Soil Geochemical Sample Locations Sample Type (1:5,000 scale)
Figure LF-02: DOK 35 AREA Detail Map Showing 2013 and Historic Compilation Showing Geochemical Samples by Type and Copper Values in PPM (1:5,000 scale)
APPENDIX 2 ALS CHEMEX ASSAY REPORTS Appendix 2.1: ALS Chemex Assay Report No.VA13165934 Appendix 2.2: ALS ChemexAssay Report No.VA13188332
Table 2: Doc 35 Area Rock Sample Descriptions
Assessment Report dated December 30, 2013 3 ITEM 1: SUMMARY
Brades Resource Corp. (“Brades”) holds an extensive land package covering several early stage porphyry and stockwork type copper-gold prospects located in the Iskut River District, northwestern BC. (the “BRC Property”). Large scale exploration programs since 2005 at Novagold Resources’ Galore Creek Project (located approximately 50 km to the south of the BRC Property), and at Copper Fox Resources Schaft Creek Property, (located approximately 45 km to the southeast of the BRC Property), have significantly increased the copper and gold resources at both projects and demonstrate the Iskut River District’s potential for large copper and gold deposits.
The BRC Property was acquired primarily by staking between 2007 and 2009. The nearest road accessible community is Telegraph Creek located approximately 40 kilometers to the north east. The physiography of the project area is rugged and at present the only way to access the property is by helicopter or float plane from Telegraph Creek or Dease Lake.
The Galore Creek Deposit is classed as an alkalic porphyry and is localized in Triassic aged andesitic rocks belonging to the Stuhini group that have been intruded by a series of late Triassic to early Jurassic aged felsic stocks and dykes. The main mineralized zones are localized within structurally controlled, potassium feldspar and biotite rich alteration zones and are flanked by propylitic alteration mineralized with pyrite. Schaft Creek is also localized within Stuhini group volcanic rocks but is classified as a calc-alkaline porphyry. Geological models for Schaft Creek show that mineralization is associated with both deep seated potassic alteration zones and within peripheral, propylitic altered stockworks and breccia zones.
Based on the distribution of regional scale stream sediment copper geochemical anomalies and published technical information concerning the various known copper-gold prospects in the project area (technical data available from the BC Minfile database) there appear to be five main areas of interest within the BRC Property. For reference, these are referred to as the DOK 35 Area, the Teck Area, the Yeti Area, the Strata Creek Area and the Yehiniko East Area.
According to the BC Ministry of Mines (BCMEM) Minfile database the known copper and gold mineral occurrences within the BRC Property exhibit mineralization and alteration characteristics typical of porphyry and stockwork type copper-gold deposits. These occurrences have been documented by various previous workers including Teck Corp., the Geological Survey of Canada, the Swiss Aluminum Mining Company, Schellex Gold Corp., and several other junior mining companies. Geological maps available online from the BCMEM confirm that the BRC Property is underlain by Stuhini Group volcanic rocks and various felsic intrusive rock units, which is the same geological setting that hosts the Galore Creek and Schaft Creek deposits. Regional scale stream sediment survey maps and regional scale airborne magnetic survey maps (available online from the BCMEM) also suggest geological similarities between the BRC Property and the Galore Creek and Schaft Creek areas.
Assessment Report dated December 30, 2013 4 Based on the potential to expand known mineralized zones and identify new areas of mineralization, Brades acquired the BRC Property and has carried out several exploration programs. Since the Property was acquired in 2007 Brades has completed an airborne geophysical survey in the Strata Creek Area, repaired an existing air strip and constructed a base camp in the northeastern part of the property (Yeti Area), completed helicopter assisted programs of geological mapping and verification sampling within the Teck Area and the Yeti Area, prepared detailed 3D elevation models for the main areas of interest and completed a detailed structural interpretation to identify the structural controls on mineralization.
Between May 1 and October30, 2013 Brades completed technical assessment work in the area referred to as the Doc 35 Area located in the western part of the BRC Property. This work included SOW No.5447737 recorded on May 9, 2013 related to technical work completed on the Teck Prospect in 2012 and four separate Statements of Work relating to technical work completed on the Doc 35 Prospect - SOW No.5453427 recorded on June 11, 2013, SOW No.5464789 recorded on August 27, 2013, SOW No.5474146 recorded on October 28, 2013 and SOW 5474763 recorded on October 30, 2013. The total cost of the exploration work completed for Brades Resources during 2013 was $115,000.
The DOK 35 Area is located in the north western part of the BRC Property and consists of three known Minfile prospects which reportedly exhibit propylitic alteration and copper mineralization in andesitic volcanic rocks. Historic technical reports document prospecting programs and widely spaced geochemical sampling programs that identified numerous gossan zones and “copper in soil” anomalies including a 400 meter wide anomaly (referred to as the DOK 35 Prospect) that exhibits values ranging from 247 ppm to 800 ppm copper.
It is also important to note that the western boundary of the DOK 35 Area adjoins a package of claims owned by unrelated parties (presently under option to Boxxer Gold Resources “Boxxer”) that cover the DOK Prospect (located immediately north of the boundary between Brades Property and Boxxer Resources Property). According to Boxxer the DOK Prospect consists of two strong copper in soil geochemical anomalies (one adjoining the property boundary and one located approximately 5 kilometers north of the property boundary) which have a strong IP response but which have not yet been drill tested. Previous exploration work at the DOK Prospect documents extensive biotite – feldspar alteration and trench sampling results of up to 0.66% copper over 38 meters. The style of alteration and tenor of mineralization reported at the DOK Prospect are similar to that encountered at Galore Creek; however, it is important to note that there is no assurance that similar mineralization will be identified within the claims that are the subject of this report. Regional stream geochemistry data shows elevated copper values in stream sediments draining the DOK 35 Area; however, the extent of the soil geochemical anomalies has not yet been determined. Additional information concerning the DOK Prospect is included in the section titled “Adjacent Properties”.
The work carried out in 2013 consisted of transporting helicopter fuel and field equipment to the airstrip at Yehiniko Lake to support the planned work program at the DOK 35 Area,
Assessment Report dated December 30, 2013 5 construction of a helicopter supported fly camp in the Doc 35 Area, compilation studies of the technical work completed on the adjoining property by Boxxer and extensive reconnaissance prospecting, soil sampling and rock sampling designed to verify historic reports which document the presence of gossan zones and soil geochemical anomalies within the claim area owned by Brades. A total of 205 soil samples and 47 rock samples were collected during the 2013 program.
Exploration involved comparing the geology and alteration on the DOK 35 area to the adjoining property owned by Boxxer the north. Numerous dykes and gossanous zones were located and sampled during the program and soil grids were established to test the extent of the zones. The approximate contact between the Coast Range plutonic complex and sediment-volcanic package was also explored with some anomalous copper in soil results obtained. The extremely rugged terrain hampered the exploration program and future exploration programs will require numerous fly camps to be established for better productivity.
Because of the steep, mountainous terrain, soil grids were restricted to small areas where soil development was possible. Three separate soil grids were established, the Boundary East grid, the Boundary West grid and DOK 35 grid. The first small grid, (referred to as Boundary Grid East), is located on the north facing slope of a large scree slope beneath the majority of the gossanous outcrops. A total of 48 contour samples were collected along the sparsely vegetated slope with samples returning values up to 1,060ppm copper (sample 1,149,001). The zonation of anomalous copper value in soils on the east side of this grid correlate with the syenitic dykes directly upslope. The west side anomalies are related to pyritized shears and faults. The area is predominantly rusty, mafic volcanics with extensive shearing and faulting. Shears are infilled with barite, quartz and carbonates with varying amounts of pyrite and chalcopyrite. A total of 12 rock samples that were collected from the area directly upslope from the soil grid are currently being assayed and may clarify the anomalous soil values.
The second grid, Boundary Grid West, started near the contact of the Coast Range intrusives and encircled the ridge of the mountain along elevation contours. 62 soil samples were collected from three lines between the 1100m and 1150m elevation contours. The soils show a weakly anomalous zone near the intrusive contact with the country rocks but the majority of the soils were below anomalous levels. Four rock samples were collected along a shear zone within the intrusive rocks that contained minor amounts of chalcopyrite and pyrite accounting for the small soil anomaly.
The third grid, (referred to as the DOC 35 Grid), is located near a historic rock sample 2951 (Aris 30706) with 1.1% copper and 42.3g/t silver. The grid is along the base of a south facing slope, covering the contact between the syenitic intrusive rocks and dioritized sediments. The grid confirmed the large anomaly (referred to in Aris 30706) near the eastern portion of the grid, along the contact of the intrusion into the sedimentary rocks.
Assessment Report dated December 30, 2013 6 ITEM 2: INTRODUCTION AND TERMS OF REFERENCE The Author was requested by Brades Resource Corp. to review all available historic technical information for the BRC Property and the surrounding area; to supervise completion of a preliminary exploration program on the BRC Property and if warranted, to plan and recommend a follow-up program to explore the mineral potential of the claims. Brades Resources Corp. intends to utilize this technical report in support of an application to the TSX Venture Exchange for an Initial Public Offering.
Sources are listed in the Terms of Reference section of this report and are cited where appropriate in the body of this report. The reports listed in the Terms of Reference section of this report appear to have been completed by competent professionals without any misleading or promotional intent.
The qualified person who is the Author of this report worked on various exploration projects in the Galore Creek area between 2002 and present for several junior resource companies. The Author visited the BRC Property several times between 2007 and 2009 and again between September 23 and September 26, 2012. I have worked as an exploration geologist for a total of 23 years since graduation from University. I have extensive work experience in western and northern Canada and in Mexico. I have worked on several copper - gold projects in northwestern British Columbia. I personally supervised all of the exploration work carried out by Brades Resource Corp. between August 2007 and October 2012.
ITEM 3: RELIANCE ON OTHER EXPERTS
The Author has prepared this report based on information which is believed to be accurate but which is not guaranteed. The available technical data for the BRC property consists of regional geological and airborne geophysical information compiled by the BCMEM and documentation regarding field investigations completed within the claim area by various previous workers including Teck Corp., the Geological Survey of Canada, the Swiss Aluminum Mining Company, and various other field geologists and junior mining companies.
The main source of regional geological information concerning the project area is Bulletin 92 and Bulletin 104 published by the British Columbia Ministry of Energy and Mines. The Author has no reason to doubt the accuracy or completeness of the contained information.
To the best of the Author’s knowledge, there are no known existing environmental liabilities to which the property is subject, other than the requirement to mitigate any environmental impact on the claims that may arise in the course of normal exploration work and the requirement to remove any camps constructed on the BRC Property or any equipment used in exploration of the claims in the event that exploration work is terminated.
Assessment Report dated December 30, 2013 7 ITEM 4: PROPERTY DESCRIPTION AND LOCATION
4.1 Location
The property is located approximately 45 kilometres south west of the community of Telegraph Creek and approximately 50 kilometres north of Novagold Resources Galore Creek Project. The approximate geographic centre of the property is situated at Latitude 57 degrees 31' 48”N and Longitude 131 degrees 26' 21”W (UTM 9N: 353700E / 6378800N). The location of the project area relative to other mining claims, access roads and other developed alkalic porphyry copper- gold prospects is illustrated in Figure 1.
4.2 Property Description
The original BRC Property consisted of 38 contiguous map staked mineral titles which form an irregular shaped block comprising 14,113.50 hectares. Figure 6 shows the location of each of the claims relative to generalized topographic features and the main areas of interest described in the Summary section.
The Company initially acquired a 100% interest in the Property by direct purchase and staking between April of 2007 and September of 2008. On December 16, 2011, 13 peripheral mineral tenures of the original 38 mineral tenures comprising the BRC property were allowed to lapse and were re-staked to reduce claim assessment work requirements. On December 24, 2011, one additional tenure was staked, increasing the total mineral tenures for the BRC Property to 39, now comprising of 14,113.50 hectares. The following table is a list of claims, owned by the Company , comprising the Property effective October 30, 2013. ).
Table 1: Listing of claims, owned by Brades Resources Corp., comprising the BRC Property effective October 30, 2012.
Tenure Number Good To Date Area (ha) 556978 2014/nov/02 347.4036 558764 2015/jul/01 416.8577 558765 2015/jul/01 399.6088 558766 2015/jul/01 417.1014 558767 2015/jul/01 417.0498 558768 2015/jul/01 417.166 558770 2015/jul/01 434.2366 558779 2015/jul/01 417.2261 558780 2015/jul/01 417.2996 558781 2015/jul/01 434.8133 558782 2015/jul/01 434.8693 558783 2015/jul/01 435.0142 558786 2014/nov/02 435.1336 558797 2015/jul/01 433.9856 569236 2015/jul/01 435.0854 570447 2015/jul/01 469.1015
Assessment Report dated December 30, 2013 8 577682 2015/jul/01 156.44 577685 2015/jul/01 208.6578 577687 2015/jul/01 312.77 577688 2014/nov/02 156.4399 577691 2015/jul/01 52.1465 577693 2015/jul/01 260.6536 591473 2015/jul/01 312.8776 591474 2015/jul/01 416.7632 591475 2015/jul/01 433.957 937691 2015/jul/01 69.4524 937695 2015/jul/01 434.2973 937697 2015/jul/01 434.624 937699 2015/jul/01 364.5659 937702 2014/nov/02 399.4636 937703 2014/nov/02 365.0413 937704 2015/jul/01 312.5138 937705 2014/nov/02 417.2689 937707 2015/jul/01 434.8013 937708 2014/nov/02 417.445 937710 2014/nov/0215 417.5779 937712 2014/nov/02 400.1151 937715 2015/jul/01 417.2837 938777 2015/jul/01 156.3974 TOTAL: 14113.5057
4.3 Provincial Mining Regulations
The Property is owned 100% by the Company and is not subject to any royalties, back in rights, payments or other agreements. Prior to July 1, 2012 BC Ministry of Mines regulations required that title to the claims be maintained through the performance of annual assessment work filings and payment of required fees. For the first three years after a claim was staked a minimum of $4.00 per hectare in eligible exploration and development expenditures needed to be incurred. In subsequent years, a total of $8.00 per hectare in eligible exploration expenses needed to be incurred. Effective July 1, 2012 new regulations came into effect that changed the requirements from a 2-tier system to a 4-tier system and have significantly increased the minimum exploration expenditures that are required to maintain mineral tenures in good standing. Under the new regulations all mineral tenures are deemed to be in their first anniversary year and the new minimum exploration expenditures will be $5.00 per hectare for anniversary years 1 and 2, $10.00 per hectare for anniversary years 3 and 4; $15.00 per hectare for anniversary years 5 and 6 and $20.00 per hectare for each subsequent anniversary year.
Prior to July 1, 2012 holders of mineral tenures had the option of making payments equivalent to the minimum exploration and development expenditures (referred to as PIED) required by the Ministry of Mines instead of incurring the required expenditures. Under the old regulations a minimum of one day and a maximum of one year of PIED could be applied to mineral tenures. Under the regulations which come into effect July 1, 2012 the holders of mineral tenures will still have the option of making payments instead of exploration and development work however, the new PIED rate will be set at double the value of the minimum exploration and development expenditures required. In addition to the changes in the PIED rate tenure holders
Assessment Report dated December 30, 2013 9 who elect to make payments instead of incurring expenditures will need to pay for a minimum of 6 months which under the new regulations will be equivalent to the minimum expenditures for an entire year. Similar to the assessment work requirements, if a recorded holder wishes to register PIED, the claim will also be treated as if it is in its first anniversary year for the purpose of calculating the assessment requirement, as of the date of implementation (July 1, 2012).
To the best of the Author’s knowledge, government permits are required to carry out the proposed exploration programs and for any follow up diamond drilling program recommended after completion of Stage 1 and2. These programs require application to the British Columbia Ministry of Energy and Mines for permits and the Issuer may be required to post security equivalent to the estimated costs of any reclamation work which will be required after completion of the proposed exploration work. In May, 2009 the Author applied to the BC Ministry of Mines regional office in Smithers for a permit to carry out the proposed Stage 1 Program and approval was granted pursuant to Reclamation Permit MX-1-806. The exploration permit was initially valid to September 30, 2011. In June 2011 the Author applied to the BC Ministry of Mines for an extension and the Reclamation Permit has been extended to December 30, 2013.
To the best of the Author’s knowledge approval from local First Nations communities may also be required to carry out the proposed Stage 2 exploration program. The reader is cautioned that there is no guarantee that the Issuer will be able to obtain approval from local First Nations. However, the Author is not aware of any problems encountered by other junior mining companies in obtaining approval to carry out similar programs in nearby areas nor is the Author aware of any instances where local First Nations communities have objected to exploration work in the general project area.
To the best of the Author’s knowledge, none of the claims which comprise the BRC Property have surface rights. In the event that a significant mineralized zone is identified detailed environmental impact studies will need to be completed prior to initiation of any advanced exploration or mining activities. The reader is cautioned that there is no guarantee that areas for potential mine waste disposal, heap leach pads, or areas for processing plants will be available within the subject property.
ITEM 5. ACCESSIBILITY, CLIMATE, PHYSIOGRAPHY AND INFRASTRUCTURE
5.1 Accessibility and Infrastructure
Access to the BRC Property is by way of helicopter or fixed wing aircraft from the community of Telegraph Creek approximately 45 kilometres north east of the property. Figure 1 shows the location of the BRC Property relative to nearby access roads, mines and other developed prospects. It is also possible to land a float plane on Yehiniko Lake located at the north eastern corner of the property. Alternatively the claims could be accessed by helicopter from the Bob Quin airstrip located on Highway 37. Crews travelling to and from the site can stay at Telegraph Creek. Driving time to Telegraph Creek from Terrace or Smithers is approximately ten or twelve hours. Experienced field personnel and drilling contractors are available in the communities of Terrace and Smithers.
Assessment Report dated December 30, 2013 10 The only infrastructure existing in the project area is a rough airstrip located adjacent to Yehiniko Lake in the northeastern part of the BRC Property. A base camp for crew accommodation for completion of the proposed Stage 1 program was constructed on the airstrip in September of 2009. At present there is no other infrastructure in the vicinity of the subject property.
There are abundant water sources within and adjacent to the BRC Property. At present there are no power sources available at the property. Although no detailed assessment has been undertaken to determine if there are areas within the Property that could be used for tailings and or waste disposal the physiography of the north eastern parts of the Property may be permissible for such uses. The reader is cautioned that there is no guarantee that areas for potential mine waste disposal, heap leach pads, or areas for processing plants will be available within the BRC Property.
It may be technically feasible at some point in the future to either barge equipment across the Stikine River or construct a bridge across the Stikine River from existing road access to Telegraph Creek and Glenora on the north side of river and construct an access road along Yehiniko Creek a distance of approximately 30 kilometers. However, no engineering studies have been undertaken to determine costs or potential environmental impacts. The reader is cautioned there is no guarantee that construction of an access road would be approved by Federal and Provincial regulators or affected First Nations.
5.2 Physiography, Climate, Vegetation and Current Land Use
The physiography of the BRC Property is extremely rugged, outcrop is extensive along the ridges but the slopes of the creeks within the project area are generally soil or talus covered. The western part of the claim group includes the DOK 35 Area and the Teck Area and covers the southwest facing slope of Dokdaon Creek and the ridge between Dokdaon and Strata Creek. The slopes are generally steep with elevations ranging from 700 meters in Dokdaon creek to 1,500 meters on the ridge. Exposure is good in the upper parts of the ridge area but much of the slopes are soil or talus covered.
The central and northeastern parts of the claim group comprise the Strata Creek Area and the Yeti and Yehiniko East Areas and cover Quatrino Creek and the Yehiniko Creek in the eastern part of the claim area. Satellite imagery shows that the lower slopes of the creeks are covered with scrub brush and stunted spruce with the upper slopes devoid of vegetation except for alpine grasses and flowers.
The project area is in the rain shadow of the Coast Range Mountains in the boundary area of the Coast Mountain and Intermontane physiographic belts giving the area a modified continental climate typified by long cold winters and short cool summers. The average annual temperature at Galore Creek is 0.4 degrees Celsius with 2278 mm of precipitation. At Schaft Creek, 40 kilometers to the south east the average temperature is -1.1 degree Celsius with 741 mm of precipitation. The BRC Property likely has a climate similar to Schaft Creek with 700 to 800 mm of precipitation annually (50% as snow), a mean summer temperature of 6-7 degrees and mean winter temperature of -8 to -10 degrees. The property is generally free of snow for approximately four months of the year. In general, exploration work in this area is carried out from July until October. Due to limited access current land use is limited to hunting.
Assessment Report dated December 30, 2013 11 ITEM 6. HISTORY OF EXPLORATION
According to Sivertz the first Canadian geologists to explore the Stikine River area were G.M. Dawson and R. McConnell in 1887. Their reconnaissance surveys were followed up by Kerr (1924-1929) and Souther (1971) and most recently, mapping of parts of the project area has been completed by the BCMEM geologists (Brown, Greig and Gunning, 1990-1991). Exploration for minerals began in 1860 with the prospecting of the Stikine River for placer gold. Lode gold prospecting occurred concurrently with placer mining but modern base metal exploration did not begin in earnest until the 1950’s as helicopters came into general use. The important Galore Creek, Copper Canyon and Schaft Creek porphyry copper deposits were discovered in the first decade of this period of exploration beginning with Galore Creek in 1955.
During the 1980’s and 1990’s several exploration programs were carried out in various parts of the current BRC Property by various exploration companies. Based on the distribution of regional scale stream sediment copper and gold geochemical anomalies and information concerning the various known copper-gold prospects in the project available from the BCMEM Minfile database there appear to be five main areas of interest within the BRC Property. For reference these are referred to as the DOK 35 Area, the Teck Area, the Yeti Area, the Strata Creek Area, and the Yehiniko East Area.
During the early 1970’s, the Swiss Aluminum Mining Company carried out geological mapping and widely spaced soil geochemical surveys within the area referred to as the DOC 35 Prospect. This work identified numerous gossan zones and “copper in soil” anomalies including a 400 meter wide anomaly (referred to as the DOK 35 Prospect) that exhibits values ranging from 247 ppm to 800 ppm copper along with elevated molybdenum values.
In the early 1980‘s Teck Exploration reportedly identified a stockwork / vein system approximately 100 meters wide within the propylitic alteration zone that could be traced along strike for 250 meters. The stockwork / vein system is highly oxidized at surface and reportedly returned sample assays ranging from trace values to 0.05% Mo, 0.20% Cu, 10 g/t Ag, 0.8 g/t Au and 0.17% W. The reports prepared by Teck note that potential extensions of the of the stockwork zone are overburden covered.
In the early 1990’s Schellex Gold Corp. and various other junior mining companies (including Toscana Resources) carried out reconnaissance scale prospecting and sampling in the area referred to as the Yeti Prospect. Shellex reportedly identified a north trending, 300 hundred meter wide quartz and carbonate stockwork zone with copper and gold mineralization that was traced for over 600 meters.
Since the Property was acquired in 2007 Brades has completed an airborne geophysical survey in the Strata Creek Area, repaired an existing air strip and constructed a base camp in the northeastern part of the property (Yeti Area), completed helicopter assisted programs of geological mapping and verification sampling within the Teck Area and the Yeti Area, prepared detailed 3D elevation models for the main areas of interest and completed a detailed structural interpretation to identify the structural controls on mineralization.
Assessment Report dated December 30, 2013 12 ITEM 7. GEOLOGICAL SETTING AND MINERALIZATION
Author’s note: The majority of the information in this item is excerpted from Bulletin 92 and Bulletin 104 published by the British Columbia Ministry of Energy and Mines.
The Stikine River – Yehiniko Lake Area is underlain by rocks belonging to the Stikine Terrane which are part of the Intermontane Belt. The Stikine terrane includes three major groups of rocks in this part of the Iskut River District. These include island-arc volcanic and sedimentary rocks of the Paleozoic Stikine assemblage, Upper Triassic Stuhini Group marine-arc volcanic and sedimentary rocks, and Hazelton Group rocks consisiting of equivalent Lower-Middle Jurassic volcanic and sedimentary rocks. Overlapping the volcano-sedimentary rocks are various erosional remnants of the Upper Cretaceous to Eocene age Sustut and Sloko volcanic rocks.
These supracrustal rocks are intruded by stocks, plugs dikes and sills ranging in age from Mid- Triassic to Tertiary. The intrusive rocks range in composition from from diorite to granite with the larger plutons generally comprised of biotite-hornblende granodiorite. Within the project area the regional structural style involves north to northwest striking and east to northeast striking faults.
According to Bulletin 104, alkalic porphyry copper deposits occur throughout the Intermontane Belt in both the Stikine and Quesnel Terranes and are restricted to the volcanic island arc assemblages of the Nicola, Takla and Stuhini groups. The best known example of the alkaline porphyry copper deposits in the Stikine Terrane is the Galore Creek deposit located approximately 50 kilometers south of the BRC property. Galore Creek is presently the focus of an intensive evaluation by Nova Gold Resources Ltd. Age dating shows that U-Pb ages are similar (circa 200 to 210 Ma) for intrusions associated with porphyry Cu-Au deposits in both the Stikine and the Quesnel terranes. Multiple alkaline intrusions and associated ultramafic phases are also present at Galore Creek. U-Pb dates of 205.1 ±2.3 (zircon) and 200.1±2.2 (titanite) for the potassium feldspar megacrystic syenite porphyry at Galore Creek constrain emplacement ages and brackets Cu-Au mineralization.
According to the geological map available from the BC Government the western part of the BRC Property is underlain mainly by andesitic volcanic rocks belonging to the Stuhini Group. Coast Range granitic intrusive and Permian aged sedimentary rocks dominate the area to the west of the claim area. The andesitic rocks are intruded by tabular and irregular bodies of syenite and quartz porphyry (felsites). Figure 7 shows the geology of the claim area.
Assessment reports completed by the Swiss Aluminum Mining Co. on the DOK 35 Area describe extensive areas of highly fractured, propylitic altered andesites containing pyrite and scattered chalcopyrite mineralization. The best copper mineralization is developed along structural zones within areas of higher grade alteration which exhibit biotite and K-feldspar alteration.
Assessment reports prepared by Teck Corp. concerning exploration work carried out in the southwestern part of the BRC Property identified large area of granodiorite with a large pendant of Stuhini group volcanic rocks. The rock units described by Teck include volcanic breccias, granodiorite breccias felsites and feldspar porphyry’s and later andesitic and basaltic dykes that crosscut all rock types. The stockwork zones and the north trending bleached fault zones identified by Teck are localized within and along the margins of the roof pendant. According to Sivertz, 1991 the eastern part of the BRC Property is also underlain by Stuhini Group andesitic
Assessment Report dated December 30, 2013 13 rocks. These rocks are intruded by biotite – hornblende tonalite of the mid Triassic aged Nightout Pluton along the eastern side of the BRC Property.
The regional scale north, northwest and north northeast oriented faults cut the andesitic rocks and are associated with large gossan zones and areas of propylitic alteration and scattered copper mineralization. Several major fault systems are present within the property including a north-northwest system, a northeast system and a north trending system present in the eastern part of the property. All of the fault systems are reportedly steeply dipping normal faults. The northeast system is the older and is offset by the north northwest system. It appears to control the rock type distribution. The north and north-northwest fault systems may control the mineralization.
According to Blann, 1992, the Stuhini Group rocks are comprised primarily of massive feldspar crystal lithic, lapilli tuff and flows of andesite to basalt composition. Subvolcanic to hypabyssal units are common throughout the property. Augite-hornblende porphyritic basaltic andesite and feldspar (plag.) porphyritic diorite-andesite occur locally with megacrystic textures. Most of the porphyritic units are mapped as volcanic rocks, corresponding to the recent regional work done by the GSC.
According to the BCMEM online database (Minfile) the BRC Property covers eleven known copper-gold mineral occurrences (Minfile prospects) many of which exhibit mineralization and alteration characteristics typical of porphyry copper-gold deposits. The known occurrences were documented by various previous workers including Teck Corp., the Geological Survey of Canada, the Swiss Aluminum Mining Company, and various geologists and junior mining companies and have all been incorporated into the BC Minfile database. Geological maps available online from the BCMEM confirm that the BRC Property is underlain by Stuhini Group volcanic rocks and various felsic intrusive which is the same geological setting that hosts the Galore Creek and Schaft Creek deposits. Regional scale stream sediment survey maps and regional scale airborne magnetic survey maps (available online from the BCMEM) also indicate similarities between the BRC Property and the Galore and Schaft Creek areas.
Based on the distribution of regional scale copper and gold geochemical anomalies and information concerning the various known copper-gold prospects in the project available through the BC Minfile database there appear to be five main areas of interest within the DOK 35 Project. For reference these are referred to as the DOK 35 Area, The Teck Area, The Yeti Area, The Strata Creek Area and the Yehiniko East Area.
7.1 DOK 35 Area
The DOK 35 Area is located in the north western part of the BRC Property and according to BC the BC Minfile database there are 3 known prospects within this area (104G039 – DOK 35 Prospect, 104G084 – Gu North Prospect, and 104G075 – GU Prospect) which exhibit propylitic alteration and copper mineralization in andesitic volcanic rocks. Previous prospecting programs and widely spaced geochemical sampling programs identified numerous gossan zones and “copper in soil” anomalies including a 400 meter wide zone (referred to as the DOK 35 Prospect) that exhibits values ranging from 247 to 800 ppm copper along with elevated molybdenum values. It is important to note that the western boundary of the DOK 35 Area adjoins a package
Assessment Report dated December 30, 2013 14 of claims owned by unrelated parties that cover the DOK Prospect (located approximately 5 kilometers northwest of the DOK 35 Prospect). Previous exploration work at the DOK Prospect documents extensive biotite – feldspar alteration and trench sampling results of up to 0.66% copper over 38 meters. The style of alteration and tenor of mineralization at the DOK Prospect are similar to that encountered at Galore Creek however it is important to note that there is no assurance that similar mineralization will be identified within the claims that are the subject of this report. Additional information concerning the DOK Prospect is included in the section titled Adjacent Properties.
7.2 Teck Area
The Teck Area consists of a large area of alteration and mineralization originally identified by Teck Corp in 1980 located along the slopes above Dokdaon Creek in the south western part of the BRC Property. The BC Minfile database indicates that there are 2 known prospects in this area (104G058 – MARG WEST and 104G089 – MARG EAST). According to Assessment Report No.9617, Teck identified a stockwork / vein system approximately 100 meters wide that could be traced along strike for 250 meters and a north trending fault system that had undergone intense bleaching, silicification and pyritization. The stockwork / vein system is highly oxidized at surface and reportedly returned sample assays ranging from trace values to 0.05% Mo, 0.20% Cu, 10 g/t Ag, 0.8 g/t gold and 0.17% W. Samples from the north trending fault zone reportedly ranged from 0.03 to 1.26% Cu, 6 to 110 g/t Ag and trace to 2.6 g/t gold. The assessment report prepared by Teck Corp. notes that potential extensions of the of the stockwork zone are overburden covered and also notes the presence of several different intrusive and volcanic breccia units. Regional stream geochemistry data shows elevated copper values in stream sediments draining the Teck Area. The overall size of the gossan zone and the presence of the various breccia units noted by Teck are consistent with typical porphyry copper style mineralization and there is no record of any detailed follow up exploration in this area other than verification sampling carried out by Brades. Figures 10 and 11 and 3D perspective views of the Teck Area .
7.3 Strata Creek Area
The Strata Creek Area is located in the central and north eastern part of the BRC Property and according to the BC Minfile database there are five documented prospects within this part of the claim area (104G136 – PLAYER, 104G134 – PLUM, 104G135 MUFFLE, 104G129 CHUCKSTER and 104G112 – YEHINIKO WEST). Regional stream geochemistry data shows elevated copper values in stream sediments draining the Strata Creek Area however, the most important of these Minfile prospects is believed to be the one which is plotted in the northeastern part of the claim area. According to Souther (GSC Paper 71-44) there is a large alteration zone containing copper mineralization that appears to be related to a north trending fault zone. There is no published record of follow-up exploration work on this prospect.
7.4 Yeti Area
The Yeti Area is located in the east central part of the BRC Property and covers a single Minfile prospect (104G127 - BROWNIE). According to Sivertz, 1991 this area hosts a north trending, 300 meter wide quartz and carbonate stockwork zone that has been traced for over 600 meters. The veins are reported to be variably mineralized with gold and copper and reported sample results from veins within the zone range from several hundred ppb to 24 g/t gold. Copper is
Assessment Report dated December 30, 2013 15 reported as chalcopyrite or copper oxides throughout the stockwork zone and sampling reportedly returned several samples that contained in excess of 1% copper. This part of the property was acquired after the 2007 work program was completed and was visited in September 2010. Representative chip samples collected by the Author across widths of 1.0 to 2.0 meters within the stockwork zones returned copper values ranging from 0.415% 1.940% copper and gold values of up to 0.467 g/t and confirmed the presence of significant copper and gold mineralization. Figures 8 and 9 are 3D perspective views of the Yeti Area.
7.5 Yehiniko East Area
The Yehiniko East Area consists of a single Minfile prospect (104G111 – YEHINIKO EAST) plotted within the south eastern part of the BRC Property. According to the Minfile database this prospect also consists of a large alteration zone identified by the GSC. According to Souther (GSC Paper 71-44) there is a large alteration zone containing copper mineralization that occurs around the contact between the Yehiniko pluton and the Stuhini volcanics.
ITEM 8 DEPOSIT MODELS
8.1 Characteristics of alkalic and calc alkaline porphyry and stockwork copper-gold deposits (Reference BCEMPR Bulletin 092)
Alkalic and calc-alkaline porphyry copper-gold deposits occur throughout the length of the Intermontane Belt in both Stikinia and, Quesnellia (northern and central BC). These deposits occur either within intrusive rocks or in volcanic and sedimentary rocks associated with the intrusive bodies. These types of deposits are common in the Iskut River District comprising over 25% of the reported mineral occurrences. In these deposits chalcopyrite and other copper minerals, pyrite and molybdenite occur in low grade fracture fillings and in disseminated form. Gold may be a minor but still significant component.
These types of deposits tend to occupy brecciated and faulted zones related to extensively altered subvolcanic intrusions and their volcanic host rocks. Alteration patterns for alkali type porphyry deposits are distinctly different from those of classic calcalkaline deposits which are characterized by concentric phyllic-argillic-propylitic zones. The alkalic deposits typically have a central potassic-or sodic plagioclase zone which passes outward into a propylitic zone. These often overlap and are overprinted by retrograde metasomatic alteration. Magnetite breccias and disseminations are associated with the potassic alteration zone, which hosts most of the copper and gold mineralization. Disseminated pyrite and minor copper mineralization mantle the propylitic alteration zone.
8.2 Description of the Schaft Creek Deposit
The Schaft Creek deposit is one of the largest copper-molybdenum deposits in BC. It is a calc- alkaline type. It is located approximately 40 kilometers southeast of the BRC Property. The deposit is localized near the intrusive contact between the middle Jurassic aged Yehiniko pluton and the late Triassic Hickman Intrusive complex and is hosted mainly by Stuhini Group volcanic rocks. The mineralization occurs in two north trending zones one of which is an intrusive tourmaline breccia pipe.
Assessment Report dated December 30, 2013 16 According to project operator Copper Fox Metals Inc. Schaft Creek hosts 1.393 billion tons of measured and indicated resources at a grade of 0.25% copper, 0.019% molybdenum, 0.18 g/t gold and 1.55 g/t silver.
8.3 Description of the Galore Creek Deposit
The Galore Creek Deposit comprises multiple zones of copper-gold-silver mineralization localized within breccias zones, stockworks, veinlets and disseminations within or adjoining a series of Upper Triassic aged dioritic to syenitic intrusions.
According to Novagold Resources the Galore Creek deposit is one of the largest undeveloped copper-gold-silver deposits in North America. It is an alkalic type porphyry occurrence located approximately 50 kilometers south of the BRC property.
According to project operator Novagold Resources the deposit hosts proven and probable reserves of 6.8 billion pounds of copper, 5.5 million ounces of gold and 102 million ounces of silver.
Assessment Report dated December 30, 2013 17 ITEM 9. EXPLORATION
9.1 Exploration Work Completed in 2013 by Brades Resources
Between May 1 and October30, 2013 Brades completed technical assessment work in the area referred to as the Doc 35 Area located in the western part of the BRC Property. This work included SOW No.5447737 recorded on May 9, 2013 related to technical work completed on the Teck Prospect in 2012 and four separate Statements of Work relating to technical work completed on the Doc 35 Prospect - SOW No.5453427 recorded on June 11, 2013, SOW No.5464789 recorded on August 27, 2013, SOW No.5474146 recorded on October 28, 2013 and SOW 5474763 recorded on October 30, 2013. The total cost of the exploration work completed for Brades Resources during 2013 was $115,000.
The work carried out in 2013 consisted of transporting helicopter fuel and field equipment to the airstrip at Yehiniko Lake to support the planned work program at the DOK 35 Area, construction of a helicopter supported fly camp in the Doc 35 Area, compilation studies of the technical work completed on the adjoining property by Boxxer and extensive reconnaissance prospecting, soil sampling and rock sampling designed to verify historic reports which document the presence of gossan zones and soil geochemical anomalies within the claim area owned by Brades (reference ARIS 30706). A total of 205 soil samples and 47 rock samples were collected during the 2013 program.
Exploration involved comparing the geology and alteration on the DOK 35 area to the adjoining property by Boxxer the north. Numerous dykes and gossanous zones were located and sampled during the program and soil grids were established to test the extent of the zones. The approximate contact between the Coast Range plutonic complex and sediment-volcanic package was also explored with some anomalous copper in soil results obtained. The extremely rugged terrain hampered the exploration program and future exploration programs will require numerous fly camps to be established for better productivity.
Because of the steep, mountainous terrain, soil grids were restricted to small areas where soil development was possible. Three separate soil grids were established, the Boundary East grid, the Boundary West grid and DOK 35 grid. The first small grid, (referred to as Boundary Grid East), is located on the north facing slope of a large scree slope beneath the majority of the gossanous outcrops. A total of 48 contour samples were collected along the sparsely vegetated slope with samples returning values up to 1,060ppm copper (sample 1,149,001). The zonation of anomalous copper value in soils on the east side of this grid correlate with the syenitic dykes directly upslope. The west side anomalies are related to pyritized shears and faults. The area is predominantly rusty, mafic volcanics with extensive shearing and faulting. Shears are infilled with barite, quartz and carbonates with varying amounts of pyrite and chalcopyrite. A total of 12 rock samples that were collected from the area directly upslope from the soil grid are currently being assayed and may clarify the anomalous soil values.
Assessment Report dated December 30, 2013 18
The second grid, Boundary Grid West, started near the contact of the Coast Range intrusives and encircled the ridge of the mountain along elevation contours. 62 soil samples were collected from three lines between the 1100m and 1150m elevation contours. The soils show a weakly anomalous zone near the intrusive contact with the country rocks but the majority of the soils were below anomalous levels. Four rock samples were collected along a shear zone within the intrusive rocks that contained minor amounts of chalcopyrite and pyrite accounting for the small soil anomaly.
The third grid, (referred to as the DOC 35 Grid), is located near a historic rock sample 2951 (Aris 30706) with 1.1% copper and 42.3g/t silver. The grid is along the base of a south facing slope, covering the contact between the syenitic intrusive rocks and dioritized sediments. The grid confirmed the large anomaly (referred to in Aris 30706) near the eastern portion of the grid, along the contact of the intrusion into the sedimentary rocks.
All soil samples collected by Brades Resources during 2013 were submitted to ALS Chemex in N. Vancovuer and results were reported in October of 2013. Detailed petrographic studies of the rock samples were undertaken however samples have not yet been submitted for assay.
Sample assay results are included in Appendix 2 and are shown in the large format figures LF-01, LF-02. Rock sample descriptions are included in Table 2.
Assessment Report dated December 30, 2013 19
Technician July 15 - August 21, 2013 Field Work: 5 days @ $475 2,375.00 Travel Expenses 186.15 DGW Consultants Invoice Aug2013 - (July 31 - Aug 15, 2013) Field Work: 15 days @ $440 6,600.00 Travel Expenses 3,097.64 Mike Middleton Invoice 212 - (July 15 - August 21, 2013) Field Work: 15 days @ $625 9,375.00 Travel Expenses 1,720.26 Crew demobilization to Vancouver Inclusive of vehicle charges, crew wages, and travel expenses 2,197.31 Field crew accomodation charges 46 mandays @ $65 per day 2,990.00 Petrographic work on Rock Samples Collected from DOK-35 Project Carl von Einsiedel October 10-October 30, 2013 27 hours @ $120 3,240.00
Listing of Field Equipment Rentals and Helicopter Mobilization of helicopter fuel and custom build fly camp modules for DOK-35 project (May 5- 12, 2013) CDN Ram Explorations Truck Rental (May 5-12, 2013) 2005 F250 4x4 HD extended cab (modified for offroad operations) 9 days @ $125 1,125.00 Vehicle Usage 3,651 km @ $0.45 1,642.95 DOK-35 Field Program July 15 - August 21, 2013 Ram Explorations Truck Rental (pro-rated usage July 15 - August 21, 2013) 2005 F250 4x4 HD extended cab (modified for offroad operations) 36 days @ $125 (pro-rated 33% with other Iskut River Projects) 2,970.00 Vehicle Usage 4,362km @ $0.45 (pro-rated 33% with other Iskut River Projects) 1,295.51 Ram Explorations Truck Rental 2007 Ford Ranger (modified for offroad operations) 36 days @ $95 (discounted 50%) 1,710.00 Vehicle Usage 4308km @ $0.35 (discounted 50%) 753.90 Ram Explorations Motorhome Rental (modified as emergency first aid station) 36 days @ $130 (pro-rated 33% with other Iskut River Projects) 3,088.80 Vehicle Usage 3,944 km @ $0.45 (pro-rated 33% with other Iskut River Projects) 1,171.37 Helicopter Charter Costs May 1 - August 21, 2013 Pacific Western - Helicopter Charter Helicopter Mobilization allowance (allocated 100% to DOC-35 project) 1.0 hours @ $966 966.00 Pacific Western - Helicopter Charter Invoice 30455 - May 8, 2013 1.6 hours @ $1,550 (allocated 100% to DOC-35 project) 2,480.00 294.4 litres @ $1.77 521.09 LakeLSE - Helicopter Charter Invoice 4203 - August 6, 7, 8, 9, and 10, 2013 8.8 hours @ $924.90 / hr (pro-rated 50% with other Iskut River Projects) 4,069.56 Fuel (pro-rated 25% with other Iskut River Projects) 827.64 Pacific Western - Helicopter Charter Invoice 30842 - August 3, 4, and 12, 2013 5.9 hours @ $966 / hr (pro-rated 25% with other Iskut River Projects) 4,274.55 2.3 hours @ $1,550 / hr (pro-rated 25% with other Iskut River Projects) 891.25 Fuel (pro-rated 25% with other Iskut River Projects) 1,454.67 LakeLSE - Helicopter Charter Invoice 4227 - August 19, 2013 6.9 hours @ $924.90 / hr (pro-rated 50% with other Iskut River Projects) 3,190.91 Fuel (pro-rated 50% with other Iskut River Projects) 648.95
Listing of auxilliary Field Equipment Rentals and Consumable Supplies DOK-35 Project May 1 - October 30, 2013 CDN Chainsaws, construction tooling for helicopter pad and fly camp construction, sampling tools, augers, etc 36 days @ $50 (pro-rated 33% with other Iskut River Projects) 1,200.00 Navigation equipment, GPS’s, SPOT emergency locator (4), VHF radio’s (4) GPS, VHF and SPOT GPS emergency locator: 36 days @ $45 per day (pro-rated 33% with other Iskut River Projects) 1,080.00 Satellite telephone (backup system and emergency use only) Satphone rental: 36 days @ $20 (pro-rated 33% with other Iskut River Projects) 480.00 Satphone usage 535.00 Emergency camp rental, genset rental, survival equipment 36 days @ $75 (pro-rated 33% with other Iskut River Projects) 1,800.00 Field crew labtop and printer complete system: 36 days @ $15 (pro-rated 33% with other Iskut River Projects) 360.00 Emergency first aid equipment (BC Level 2 required to meet BC Mines Requirements) 36 days @ $55 (pro-rated 33% with other Iskut River Projects) 1,320.00 Bear deterrent, flares, Personal bear protection 36 days @ $25 900.00 Helicopter Fuel (from stock) 630 Litres @ $1.95 1,228.50 Drum Fee: 3 drums @ $50 150.00 Lumber and Plywood for tent frames 900.00
ITEM 10: DRILLING
No drill testing was carried out by Brades on the BRC Property. There is no published record of any drilling completed within the boundaries of the present property.
ITEM 11: SAMPLE PREPARATION, ANALYSIS AND SECURITY
As noted in Section 9. Exploration soil and rock sampling was carried out by Brades at the DOK 35 Prospect to confirm the presence of copper – gold mineralization reported by previous exploration companies. For this program soil and rock samples composite grab samples and chip samples were collected from within anomalous or mineralized areas believed to correspond to the approximate areas sampled by previous companies.
All samples collected on behalf of Brades from the BRC Property were sealed in plastic sample bags and shipped by bonded commercial transport to ALS Chemex in North Vancouver. No employees of Brades were involved in the sample handling or technical work completed on the BRC Property.
All soil samples were prepared and analyzed by ALS Chemex. Soil samples were dried, sieved to -100 mesh and analyzed by ICP 41 for copper and a suite of 35 elements. Assay reports are included in the Appendices which accompany this report.
All rock samples collected from the DOK 35 Area during the 2013 are currently undergoing detailed petrographic and analytical testwork and will be reported on as part of a follow-up SOW.
Standard QA and QC procedures including one blank and one standard in each 20 samples were implemented by ALS Chemex and the variability of all reported analyses was within acceptable industry standards.
In the Authors opinion the sample security employed by the field personnel involved in the sample collection and the sample preparation and analytical procedures employed by ALS Chemex are adequate for the exploration program carried out by Brades on the BRC Property. ALS Vancouver is in compliance for the requirements of ISO 9001:2000 through February 12, 2011 (ALS Laboratory Group, 2009).
ALS Vancouver is accredited through the Standards Council of Canada (SCC) for Metallic Ores and Products Mineral Analysis testing for several techniques including Fire Assay with an Atomic Absorption (AA) finish, Fire Assay with a gravimetric finish and ICP-AES using a four acid digestion.
ITEM 12: DATA VERIFICATION
As noted in Item 9 Exploration the only sampling that has been carried out by Brades are several verification sampling programs designed to confirm that significant copper and gold
Assessment Report dated December 30, 2013 24 mineralization is present within the DOK 35 Area within BRC Property. The results of the verification sampling completed in 2013 have confirmed the results reported from the DOC 35 Area reported by the Swiss Aluminum Mining Company.
Extensive additional sampling and detailed geological mapping will be required to define the overall extent of mineralization within these areas.
Details of this sampling program including sample preparation and sample analysis procedures are described in the preceding Item 11.
ITEM 13: MINERAL PROCESSING AND METALLURGICAL TESTING
No mineral processing or metallurgical testing has been carried out on samples from the BRC Property.
ITEM 14: MINERAL RESOURCE AND MINERAL RESERVE ESTIMATE
No defined body of potentially commercial mineralization has been identified to date on the BRC Property and therefore no resource or mineral reserve estimate has been completed.
ITEM 15 -22: ADVANCED PROPERTY DISCLOSURE (NOT REQUIRED)
ITEM 23: ADJACENT PROPERTIES 23.1 DOK Prospect
It is important to note that the western boundary of the DOK 35 Area adjoins a package of claims owned by unrelated parties that cover the DOK Prospect (located approximately 5 kilometers northwest of the DOK 35 Prospect). The DOK Prospect is described in the BC Minfile database as Occurrence 104G043 – DOK. Previous exploration work at the DOK Prospect documents extensive biotite – feldspar alteration and trench sampling results of up to 0.66% copper over 38 meters. The style of alteration and tenor of mineralization at the DOK Prospect are similar to that encountered at Galore Creek however it is important to note that there is no assurance that similar mineralization will be identified within the claims that are the subject of this report.
ITEM 24: OTHER RELEVENT DATA AND INFORMATION There is no other relevant data or information concerning the BRC Property. There is no additional information or explanation necessary to make the technical report understandable and not misleading.
Assessment Report dated December 30, 2013 25 ITEM 25 / 26 CONCLUSIONS AND RECOMMENDATIONS
Geological maps available online from the BCMEM confirm that the BRC Property is underlain by Stuhini Group volcanic rocks and various felsic intrusive units which is the same geological setting that hosts the Galore Creek and Schaft Creek deposits. Regional scale stream sediment survey maps and regional scale airborne magnetic survey maps (available online from the BCMEM) also indicate geological similarities between the BRC Property and the Galore and Schaft Creek areas.
Based on the distribution of regional scale copper and gold geochemical anomalies and information concerning the various known copper-gold prospects located in the project area (technical data available through the Provincial Minfile database) there appear to be five main areas of interest within the BRC Property. For reference these are referred to as the DOK 35 Area, the Teck Area, the Yeti Area, the Strata Creek Area and the Yehiniko East Area.
It is also important to note that the western boundary of the DOK 35 Area adjoins a package of claims owned by unrelated parties (presently under option to Boxxer Gold Resources “Boxxer”) that cover the DOK Prospect (located immediately north of the boundary between Brades Property and Boxxer Resources Property). According to Boxxer the DOK Prospect consists of two strong copper in soil geochemical anomalies (one adjoining the property boundary and one located approximately 5 kilometers north of the property boundary) which have a strong IP response but which have not yet been drill tested. Previous exploration work at the DOK Prospect documents extensive biotite – feldspar alteration and trench sampling results of up to 0.66% copper over 38 meters. The style of alteration and tenor of mineralization reported at the DOK Prospect are similar to that encountered at Galore Creek; however, it is important to note that there is no assurance that similar mineralization will be identified within the claims that are the subject of this report.
As noted in Item 9 Exploration soil and rock sampling has been carried out by Brades during 2013 to confirm historic reports of copper mineralization within the DOK 35 Area within BRC Property. The results of the verification sampling completed in 2013 have confirmed the historic results reported from the DOC 35 Area (reference Aris 30706). A follow-up program consisting of systematic soil sampling and detailed geological mapping is clearly warranted.
Assessment Report dated December 30, 2013 26 ITEM 27 SOURCES OF INFORMATION
Bulletin 092: Logan, J.M., Koyangi, V.M., (1994): Geology and Mineral Deposits of the Galore Creek Area, B.C. Ministry of Energy and Mines.
Bulletin 104: Logan, J.M., Drobe, J.R., McLelland, W.C., (2000): Geology of the Forrest Kerr – Mess Lake Area, North Western British Columbia, B.C. Ministry of Energy and Mines.
Blann, D, Assessment Report No.22773, Geological Report on the Yehiniko Property, dated October 1992, Toscana Resource Corporation.
Folk, P.G., Assessment Report No.9617, report on the Geology, Trenching and Sampling of the Marg and Dok Claims, October, 1981, Teck Corporation.
Greig, C.J., (2009) 2008 Exploration, Dok Property, Dokdaon and Strata Creeks, Telegraph Creek Area (N.T.S. 104G052 and 104G053), Liard Mining Division, Northwestern British Columbia, by C.J. Greig M.Sc., P.Geo., and S.T. Flasha B.Sc., March 3, 2009
Hanspeter S., Assessment Report No.3846, Report on a Geological Survey done on the PR Group (Empire Metals Property), dated September 1972, Swiss Aluminum Mining Company.
Hanspeter S., Assessment Report No.3847, Report on a Geological Survey done on the GU Group (Empire Metals Property), dated September 1972, Swiss Aluminum Mining Company.
Ostensoe, E., Assessment Report 21168, Report on the Yeti 4 – 7 Claims, Yehiniko Lake Area, dated December 15, 1990, prepared for Toscana Resources Ltd
Sivertz, G., 1991, Assessment Report No. 21302, Assessment Report on the Yeti 1-3 Claims, dated May, 1991, Schellex Gold Corp.
Ulrich, G.D., Assessment Report No.3238, Report on Geological, Geochemical and Geophysical Surveys and Physical Work on the Empire Metals property (under option to the Swiss Aluminum Mining Company), dated August 4, 1971.
Veitch, J., Assessment Report No.3029, Geological Report on the DOK 1-36 Claims for Canadex Mining Corp., September 21, 1970.
Whittles, A, Assessment Report No.24970, Air Photo Interpretation Report on the Yeti Claim Group, Yehiniko Lake Area, April 29, 1997, Gold Win Ventures Inc.
According to the BC Ministry of Energy and Mines online database (Minfile) the BRC Property covers eleven known copper-gold mineral occurrences many of which exhibit mineralization and alteration characteristics typical of porphyry copper-gold deposits.
Internet Sites
Note: all data from BC Ministry of Mines downloaded from: http://www.em.gov.bc.ca/Mining/Geolsurv/MapPlace/geoData.htm
Assessment Report dated December 30, 2013 27 CERTIFICATE OF QUALIFICATION
I, Carl von Einsiedel, 8888 Shook Rd., Mission, British Columbia, V2V-7N1, hereby certify that:
1) I am an independent consulting geologist with an office at 8888 Shook Road, Mission, BC, V2V-7N1.
2) I am a graduate of Carleton University in Ottawa, Ontario, Canada in 1987 with a BSc. in Geology. This certificate applies to the “Technical Assessment Report for the BRC Property, north western British Columbia dated December 30, 2013 prepared for Brades Resource Corp.
3) I am a member in good standing of the Association of Professional Engineers and Geoscientists of the Province of British Columbia. I have practiced my profession as a geologist throughout the world continuously since 1987. (APEGBC – License no. 21474).
4) I have worked as an exploration geologist for a total of 26 years since graduation from University. I have extensive work experience in western and northern Canada and in Mexico. I have worked on several copper - gold projects in northwestern British Columbia. I visited the BRC Property in 2007, 2010, 2011, 2012 and again in August of 2013. I personally supervised all of the exploration work that is the subject of this report carried out by Brades Resource Corp. between July 15 and August 21, 2013.
5) I have read the definition of “qualified person” set out in National Instrument 43-101 and certify that by reason of education, experience, independence and affiliation with a professional association, I meet the requirements of an Independent Qualified Person as defined in National Policy 43-101.
6) I am responsible for the preparation of all sections of this technical report.
7) I have had extensive prior involvement with the Property that is the subject of this report.
8) I am not aware of any material fact or material change with respect to the subject matter of the technical report that is not reflected in the Technical Report.
9) I am fully independent of the Issuer applying all of the tests in section 1.4 of National Instrument 43-101. I have read National Instrument 43-101, Standards for Disclosure of Mineral Properties. This Technical Report has been prepared in compliance with National Instrument 43-101.
10) As of the date of this certificate, to my the best of my qualified knowledge, information and belief, this technical report contains all the scientific and technical information that is required to be disclosed to make the report not misleading.
11) I consent to the public filing of the Technical Report with the Ontario Securities Commission, the Alberta Securities Commission, and the British Columbia Securities Commission, any stock exchange and any other regulatory Authority and any publication by them for regulatory purposes, including SEDAR filings and electronic publication in the public company files on their websites accessible by the public, of the Technical Report and to extracts from, or a summary of, the Technical Report in the written disclosure
Assessment Report dated December 30, 2013 28 being filed, by Brades Resource Corp., in public information documents so being filed including any offering memorandum, preliminary prospectus and final prospectus provided that I am given the opportunity to read the written disclosure being filed and that it fairly and accurately represents the information in the Technical Report that supports the disclosure.
12) As of the date of this certificate, to the best of my knowledge, information and belief, the Technical Report contains all scientific and technical information that is required to be disclosed to make the Technical Report not misleading.
Dated at Vancouver, B.C. this 30th day of December , 2013.
“Carl von Einsiedel”
Carl von Einsiedel, P.Geo.
Assessment Report dated December 30, 2013 29
J n -J: --t ie-o.9, - [l A a) v -Ere: z + j' c = ,'- E O No ED o < c)f, v t! f, ()
lo € a € arD € p 6@ ::.) @ o (-) pT OJ l o 3
--.1 zcoi 14oz=6) KA€ O,zt - z-: U sruY n @vr o o zj{
e € € p
@ go .l.lo's p Aorr-j r@c)N:: o!^':() N.^NN^. -joc)ocr "()o(l [!@@@ 5 ! o () yl () (> <) c) \/ () () () () () o 3
rc)oo() (l
oo)5o : @!@@r- :lor:
N@;:@! tu!;;!N : f1 q oloro-1 ..5 0 N;a oo-oi:i X -o!.. NOA!@ @@@o! @@@o>< -,1 oo5s6 ooN- :: *-EoJ Y; + r@@i]o ;joooo q- ;;oo;i:-l o@!o -: <) 6y3 !@!5.. o a N 5,. Jioo\@@ asSgB o@o)@i; I IPEE- U 9d.5,* P i'^; ooocJ() ()i L ri i-]>-= 5 .-v<)6' ' !wi,6U) @@@@ A;;;; D - q @@@@\o Q@oQ() @@@@@ sa555 55555 @@@@@ Q@a@@ @@@@ a@@@@ 3 -l o OOOO<) ,?11:?51? OOOOO m OQ@\ - oa@\o o@@\ol c) () c) () () o UAWN_, ()@@\ o E o 5', a rc f l. fD t !. n 5 p! (o g a o f,O a p r<-l o 60 l3 @ PZN } l 1-1-.1 oio r ' rN | \ j () () () () cJ p o a O @ ..INN)N N N N.r.l NNNN.-\ r-!N_rr ooN!@ !!o<)<, i,xF^- :O @
€ € o@@oo) € 3t:qs @!o)oN ooN<)@ <- c)o<)oo o<)c)()(> -€ p d a qo p ooo-iot losoo lo-lii or:i@! ....6 3 ^ul!ol lo,; ^- 3
<)()<)oo --l o(loc)o <)T NNNNN c)()c)()o () o o () c) o"<;o NNN@O NNNON NNONO E z@; i.I tJ1=o> ?o h-s6> N@ i@! o)!o)oo !@!o 9sE oA!oc) _-,.4 z w -^-E ^ F @Ur- O zVF g irol ;:@@@@ -ra()No NN@ 9il9; ai::SF ;iNoo@--oc>()a) il@ ;i N a Yi 6 o; !r) : llo -()o()c) ()o()oo a;<)oo() o<)c)()c) X zQz : - -x; !@!@N 500!: o;@@;l N@N r c)!c)o< @ij;FoX dsfds Ns:9x
oooo oo(too c)<)o<)o o-.Joo ooc)oaJ so5$5
NNNNN N5000 oT' : lt pr_ -1 |,DoN' I o_oil n=- ii +r rD @lN!O >P NO@@N @!o)N@ : P?EE g s B"""I
NNNNN NNNNN NNNNN NNNNN o<)o()() c) () () (_) NNNNN NNNNN a-.=D" o oc)oc)c) () () c) c) () c)o()c)<) <); ro =r"i^Xtt!4, , xt j .-v v(O :--oP(,4i/F l. aaa.\.t, -l @o@oo o@@@@ 455t5 A, OOOOO aaaaa @@@@@ a@@@@ 55555 3 a OOOOO OOC)OO OOOOO @@a@@ @@@o@ @@Q@o - o@@\o OOO<)O C)OOOO c)<)ooc) 9 -, () <) a) a-) <)<)()o<) - 'o vrawN! o c @ 3 ft n a f. t! i aL 'l ! ! G g o >= JO o ,"fEePa n o 6A 3 3 ooooo l ) 3339S o=<- : .\ r
@ o;d (o I o o-- a oc)c>oo ()oooo ooc)cJo VeE ;'f :L\ @ ._a i. o'> f, c) () \-!6 _rrr_rN @NANO OONNN N50@ | O !c)o!A o@oo@ NO!O o@5@N ! € € o-''ov --ooo cJoc)oo € P o p !o@5-i @o6@6 N!6X; r@!o)@ N Rrd;EI ''@!NN @@o50 @5@NO f --l *- ;frg - YgX c! - F @\Jr-^'E UA iu'lzX.F X zoz1Do x; - --r Y l1 A, il' -l .Do *-qaJ V; o >:9" }FEE: 0 n4*g ! FX^o :-+ru^Y-rwJ-!" .-vo6' ' :--o /a >wol.-,(.) .! + p @e@a@ @@@@@ s5^^b ,ANAA.\ a@aaa @@@@@ @@@@@ s5555 J I o OOOOO OOOC)O @QQ@@ @@@@@ o@@a@ o \\\\\ \oooo ooooo OOOOC) OOC)OC) OOOOO 9 oa6\o Oqu,u)v, vr!.a_Ntr 555At - o@6\O o@@\o vlawN-.-, o 5', a ) f. o X a:. n p! f a 0. tu o ;.\JrLJ r;;6 a F1< 60= 3 3 o o()oaJo oc_)()o() o<)()()() c)o()oo x<- l t oNo5..r OANNS o()c)c>c) ()<)ocfc) - A€ NA}OD -* i: o;-'I (o a q -_-ooo oc)<)c)c) $oo.r$ .r.rAAA <) <)'- <) c> () () () () o: a= NNNNN NNNpru c) > NNONN NNONN NNNNN = ;= : .-f a NfNNN a. o'> f !!NOO oNo@o !o@o@ oNli; p o o : O @ oa@o)A [ruoou $o$or Nooo{j ruru$ru rr$ru$ ruoo$g -l -- O: € oT' € p (o o o@N;i- @50a5 p !ooX! O!NNO !T oa)o5c) ;^r;-! ONtr@! DO@@() c)"o<)c) o()o<)o QOOOO <) "'- () a) c)c)ooo o!@oo - 3 <>$-'ru<> .-, --l ruru$ocr o()c)c)c) t ^ -,5 o o ! z6rD !:.I =o>tt1 O OaS6 t -^ \J(,U-- NNNNN NNNN'' NNNNN ZT.C NNNNN NNNNN NNNNN NNNNN fi wo; UO i-lzAv o<)ooN ooooo NON!O o!aoo NNO@C) o\@oo : \>o \@@ol X zQz TnJ t- --rX; y '.AAA oo,rAA oo6oo o@600 a(Iss(n o10N! 3-t; f! !, lorot;l oooo;l o)@50:; @N6C)O -\NNN@ N-l ;s:ss ooNo;; 3 --1" rDo di * @@@oo -\@oN6 ooNS@ !o-roo oT' >:o o!oo+ 60050 OA!@N @c)N@! 'D }FEE 3 s d-;,{- = :TX^.D o<)c)oc) <)oo()() <) : i,' r) i-P>- ;;go>.T vl,(] AAA-SA qr @@@@@ 45A55 55\AS @@@@@ o@@o@ @@@@@ @@@@@ --OOO OOOOO @@@@Q @@@@@ @@Q@Q 3 \!\\\ <)()()<)o ()<)o<)o ()()oc)() o N-6\O 65wN- \oooo ooooo o@@!o o@@\o a- E o o l tr. i a-'. E J a ;\J o; F t-+< ; o od 3 3 ft .Y € ooo@x ;;:N@$ € OO@)Y xoac)N N!O):A () -., !! € sslxd 6oio!6 NX@oN Noo:lx' ^! p a o p NNNNN ,-o<^- 3 <) () --l c)oooo ooc)c)() ()()o()c) <) c) ooc)oo o()o<)o ooo(fo ocroo$ oJooo c)ooc)..r (lo(>ocJ ooooo oo()oo (:)<)(roo ocJ(loo @5_rNY ..o'is oNh6 : -C1,,3'C NNNNN NNNNN NNNNN NNNNN N! !a= : fl !J ;: @-ioo oa5N. l @oaj5! oo)oo! (ooN-l *-PoJ iil-=- + ONNO! NNO@@ NNO!.J 6>: : I?EE U .< H9+,P NNNNN NNNNN NNNNN NNNNN 5_.ox^6 ooooc) PAAAA NNNNN A,CAA,T i-.-u!:' -oooo ooooc) oc)c)()<) oj r'a) ":gr , w _-u v(o ='rDp r! o .:--:^ E ^ A55AA s.tra5A D @@@@ @ @@@@@ a@@@@ s5555 A.DAS5 ASAAA O @@@@@ @@@@@ @@a@@ @@@@@ @@Q@@ 3 6 !!\!! \oooo ooo60 OOOC)O o o@@\o o@@\o uAwN-- o- o@@!o o E ft :. q) t :L ! J op l< !r;do; o oo 3 3 a ooo()o o<)oc)<) oo(foo o<)c)c)c) () lZN } c) <) c) () c)c)c)()o c) <) cl () () l <)c)c)NC) <)ooc)<) o a'9 :il - l al-a r' I op ;:?,^oll :. f c)aJcJoo ()oo()() a c)c)<)QO <)ooo<) CJCJoO(J ooc)oo ix:' ;'= : T tu 1. o'> f] ooooo p o O @ ;lrioo :@@@o @!!!@ @@@@: @@_ri-l @@;@@ 60;@s di55r@ N-\O60 @N6(n: @@il@@ ;-i!@!o .-: oN@()o d!Ns@ <- N € € I -. 4 .,.. .- € aj: q =- d : o 3 p5 o)!o)o)! NN!@C) OONON 3 --l E ?oo; i.A 9@>=o> O 9a5 -^ L'(,U-- z. I: ; -oi AO i-lzvF X 1)O X zQz MJ r tyx; rl P -l rDoN' *_ED n=- iL +t .D >. }FEE- 8 * d-*,* ::9x^.D i r., P >,- v (o >-i8Oo.'o AAI}A s, @Q@a@ @@@@@ @@@@@ 55A5t J o @@@@@ @QAQQ ! \\\\\ \\\oo N--OAA N_,C)@@ ooooo ooo)urul ur ur (rr ur ul o N.-,<)@@ \o55w E o m l o :. i !-+. ! (o a o ir5-Li s; ^ Fr:< o 60= f 3 m () YZN I c) <) <) c) () c) <) <) <) () () () () () .. A€ ) oloto c)toc)() - o:H > @ NNNNN i! i\J i! i! vioo N=< G'= I a NNNNN NNNQN oT tu> I @oN@ @oo!N ()N5N() OX.- a o O rc @ O :i''; ! € € ()o()()o c)oc)<)o € D q- : ll] qo p ()"()o() @ AC)@N oON@r cfoovv () () () () a) o I J ocr<>o$ rr , --l 'oir!ooNSc:ocr - s I () () () <) () v,;6a) : €-d ;fg n -* 9gPzL_ NNNNN NNNNN NNNNN .'C'C.'C NNNNN A-,0-,0 fi -oi : O U ixlzAv t'^..i c)o(:)@N X \>o X z.Qz --rx; Y c)()ooo c) c, () () o<)"()" goN -- .:-\NNN o; ar- @-"iu3 -< N.'INN .J; @ () o) It P a s ! ! .! o@N!;i ,: jn-';: ooo>lPP.'or66 -\ N N,r N' -l o@No! rDo i * -q, qJ Ji * o'I o oNo!o o;Qrl6 >:o )oX o : n'=h: 3 gd.",{ ::9x^.D c)o<_)oo oc)()oo ()o()cf() c) : i r\ irrrP>-" : ;;30>.rot6' , A\I\\\ p q @@@@a @@@@a 5 D} tr L l5!5A @@@@@ @@@@@ @@@@@ @@@@@ 3 a @@@\\ tu \\\\\ \\\o6 ooooo OOO)uiuj 9 N-,()@- N-<)@@ !Oer5w a E o rc n l l. o- t :L ! J ro a -< )" a5J@o f 3 a :YZN I l ():ia)e ) +w rt la!-: o;d 3 a o- c) c) <) c) () ooc)c)o c)()oc)c) 3 ()()oc)o o-\r<)J oT a o50@@ @c)!c)@ @N-r\o <)N^- VqE l a T -. !T o'>-O f ! o : O o @ c)c)or c)oooN o)o!@ c)!A(h-r !!!oo o@!@a o@@@! )ix<^- @N!O)O Y € NN5@ : € @@No5 c):i .E!! ;!@!^ <^- € c) <) (^ c) iio)@()! -'o s (o;- T :< p N@5!@ ... < 3 - o I 3 (f () () () <) .,7 6 oo()(ro ooo<)() ()ooo() o()<)c)c) NNN@N NNNNN o6.-;a) j ; 3P<=B; ._,4 z^ I x 3-- fi -oi gO i-lzvF ro ii;i @iii! ><:!-'@ i 5:Xo5 ;i @;:i:i @ 5X@c): xoNocf X zoz\>o X r- X;MJ i)- oo)@!o Noc>oo oocroc) () () () c) <) o()()cia) N-'NNN NNNNN NNNNN NNNNN $Souo uoo$ru : r1 @NN@@ @!-:Ea: --r a;il!oo NO@"N n=- Ji + NN@!! 6>. : IFEE ii Hgs,P NNNNN NNNNN NNNNN NNNNN NNNNN NNNNN N?: 4 oc)<)o() c)oc)oc) cfooaJc) oc)()<)o oc)o()o o:54 - irJf.=TX^; .-v v(O )wiilio @@Q@O a@o@@ @@@@ a.b.N55 AA5A5 o @^ @aoaa @@@@@ a@oa@ @ N-()@€ \\\\\ !\\o o ooooo OOOUre u(^urvt s N-O@ N--O@@ \ovrAa E E o l o- i' -g p ro o 3 3 o cJoc)oo oooc)o 3ZN I l OT o:o e @oo{! o;s NNNEO o!@@! -:i5 F old 3 ap a :co -' .oT a Ve€ ;J : I o e'> 3 o O tu @ O @@@@@ @@@@o !oa@! !ooo: 'oT ..r@!oij -'9<. O Y € € .oT € o<)<)c)() ai: {- D : (o o q p !o)o!(^ 6000: .., T N!N-^; oso\o Ni I>x a f -l -! <-p ;A gr<=6> 6 - Orzt9zr.=-w n E \.,, r- (f U i,"lzVF X zvz1)o X r- --rx :-.-.; l! qJ .DoN. -J *-EqJ Y; + d>:o SPEE - Q n4*g : Tx^o i-P>l .'vo6' , >-i9On !- - 3' 9 o o 't o g o J t4 ao F o+=: io q 'o ^ -L -\ 9J .-O f !'> o O a @ o 9J Y a AJ € ll :' or -l Nd m€ /D A' i o-: N crl AJ P_ FP q,' " X(o -: rr)o* "'D oxu' => ! €;E i-H3-i J91i' !w-' I h--l rt- + 3- -r= i j -a !3;- ru= g. A X;^u Z; r) vrtivd- _ l!:. 5 n'Oc! E >l < '" j p f! o a (D --l U J!J p- 6tD 5 N o ON p rN!5 NNONf, NJNNN N!OON N-r!oN NNN -! *a O: € € € )c)() () <) c) c) c) p : (o o po- 111 xoo() -l <)ooc)Q c)oo'-o - <_) () () () o()o<)o <)'-'- ^r;i-ic) c) 3 --l :-)-:o oo$[o ()()()o() ooc)o:i c)Y-.-_)/ '-! Fx ^ iiiiooit "' :J " :.i ! zoo; ;I ilr<=oo> e 9sq $uuo$ NNNNN sru{[o '-NNNN '-NNNN NN'-ND NNNNN :-\l n @\.rf- : :I s;inoo oocJcJo ooc)().,\ c) ().\ () ..r c)cJc)oc) () c) () () c) ..7 X NNNNN NNOOS c)Nro@ @!o()() N!N@O o)oo)oa :; 50000 !oooN ll -r.-rNN5 !|.|-\N N; oNioS ;i@@-:@ (Di@@N @!500 50 <@5 ':!o:o cl.ii;P9 -r'-\@oo I 9E+--EFr (n!i;@o ooooo l?v3 NNN!@ i:81t| rwE,X o50 NDtjc)o --^"1 >f:; ^'-h- 8 R a;,{ J i'^; oa)c)oaJ ) C) c)(tc)o() = o()<)o <):;;rl i-X>-o.5 ' : .-v ' )ui.iU) ooooo ooooo ooooo ooooo ooooo oooo6 oooo o ooooo \\\!\ OJ - ooooo oooool ooooo ooooo \\\!\ \\\\\ 3 @@@@@ @@@@@ eaooa ooooo ooooo oooo o) ooooo - ro @@@@@ @o@o@ o@@Ge @oo@ o oaoao NNN)NJN) o - n wwwww o 3', E AAAFA ! \\\\\ \\\\\ \\\\\ \\\\! /D NNNN.., '-.\\oo\\\\\ \\\\\ \\\\ \\\\! l NO\UN C)\urNO OOuu,e \ tr. eoeoe !6NO\ vl NO!q NO\Ul N ()\uNO ! t! a OTO9O o<)(^Orn O6OUO eo6c)h ()ur \VlNC) i OeO uourc) C)urO\^() !. 't ! (oD g tu J6 o Dd t/l -t-.<*T oo 3 3 3zN - a e l o:o -:@ n odd a : (o or= ; p o 6ex - ., *' a !N!@@ Nx. J ; T a _a 41. !T q'> l c)oooo ooooo ooc)c)() o p : O rc @ @ O i,x,5-- ! € !;-i@@: ;1 oQro 'r.-r o N N € !;trOK X!;-t@ 55@@ ()N to@ !!;::@ € o5!!o; @ooN @oc)6c) ;-i:oN-. .,6 <- o(i(noc) ooooc) c)!o!@ :l :: -i p (o o po- rN@@( _-.6 <^- o 3 --l -roc)oo oooo<> ooc)o.i ()d;o -E : <@; L Vl=oo> 6> O U-s -^ Oqn0-w >a^ @o)oaJ6 SNNNN ; : ? noo-oi X i-lzVF !ox(no .;c)Loo X ooooc) ()oo<)<) ooo()(J o<)ooo ooc)()() ooN-rf !o!ao o@50) (fcJcJoci o;eo- NNNNN NNNNN NNNNN t,C-A't '3.,0-'3 -{,'0.'0 :: r1 qJ oNo-i;i ONOON i"! : n; -!0r P;39E+t N@5@N ;1s3d !@oao ruo,X :'oG u 59+,H 3 c {x^6 NNNNN NNNNN NNNNN NNNNN NNNNN NNNNN NNNNN c)oooo oc)()c)c) ooo(fo i-J>- .-v oro :-"|,D ' PwoL-:Ep^ ooooo oooool ooooo ooooo ooooo ooooo) ooooo ooooo o \\\\\ \\\!\ -,1- ooooo ooooo\\\\\ ooooo\\\\\ ooooo\\\\\ ooooo \\\\\ \\!\\ \\\\\ @@@@@ @@@@@ ooooo ooooo ooooo @@@@@ @@@@@ @@@@@ @@@@@ @@@@@ @@@@@ - NNNNN 6- vrvrylqu vr vr vl vt \/l awwww - wwaww ww4ww o : E sAAA} !5AA5 o \\\\\ \\\\\ \\\!\ \!!\\ !\\\\ \\!\\ n tu ..\\oo \\\\\^t555 l. NO\9N C)\UINC) N()\ NNN..,.-, 0 urC)5Ovr \ur ur!O!v NC)!urNr ()\vrN() \vrNc)\ urN()\\/ C)vtOuC) ur () \r1 () r/' OurOurO \nC)urC)u ()ur ()eO () (/r () (rj !. .t t u' C) ur C) ul C) ! l g a l< a o l::<-t 6d o 3 l I (:()ooo <) <> () c) c) oc) @ ! @;i d + @=x l a ocJooo ocJc)oc) oo()<)() ()c)c)oo = o :I a> o = O @ ;';i@ --f O or@-r@ oNo-o <- .) : ! {€ T E () <) (: =- p (o q p T on@@@ !!aAI oooil olioo @!!@! NOA@O NO@N@ ;d;\S o!lo-l s iiliJp d 3 f --l T <@; ; :. 6@>=@> P !!@= - OvrU z-: aF noo@\.rr- l1 A'- N'J o-:.D^' P;39E+ NO,x >f x o I n5 3 -p e 69+3 ::X^D nryJl-v(o FiSOn.T ooooo ooooo) ooooo ooooo ooooo ooooo o6000 wwaww o \\\\\ \\\\\ \\\\! \\\!\ \\\!\ \\\\! \\\\o ooooo ooooo ooooo \\\\! \\\\! \\\\\ 3 OOOO@ @Q@QS ooooo ooooo ooooo o @@@@@ a@@@@ @o@@o @@@@@ @@QQO OC)OO\ \\!\\ \\\\! \!!!! o OOOOUI vr ur ur vr ul \\\vrul @ Y. Y'T 5) q) () c) () <) () o E o 55t\J: \\\\\ \\\\\ 5NN\N n 6 \oooo\\\\\ \\\\\ \\\!\ \\!\! \\!\\ \!\!\ 9NO\9 NO\UTN ()\eNC) N-,,\o) OOOvr(/r t. l \UI NO! C)\u!<)\ o Oe()vr O u'ourour () (,r O ur <) Our<)q() ; <) vl C) C) u' a)L^<)ero a-+. ! J oD o J6 ,.r:JDi oQ- 3 f c)()ooc) l c)ooo() ooc)c)c) <)oo()c) () () () () .. A€ o=zN <) "-< r =o - - =! a I I @aY a sAAps, oo$jcr oi >= a Ni!i!AN NNNNS *3@,; = a a NNNNO NNNNN !@N!O @@oao o 'l' o'> !NO@! 50<)o! a -.r c) (t c) NOIjC) @'.roN! 5!!o@ oNo\o !oooc) ooNc)o o o= o 6 @ .' ..'., N : !@o*o o!5@ : s€ € ooooc) c) (l c) <) () ! p (o g g ooooo ooooo <)jorl o I 3 --l ooN<> ONNN sooS:i N@!N5 D@<)@ti ao :@@ ::@@!o @NialN <@!No l Tl gr_ p-..'o i N'J HS;;g o6!oi; HF+ t9 1y ooo<) oooo<) O!@rO ruE,: :'o,;_n f .. u li'-t XgsB !:rx^o i-I>- .-v ot6 ' ' Dwi.il-i! ooooo ooooo oooo wwaaw oooo o ooooo C']oooo ooooo) ooooo \\\\! \\\!\ \!\\ wwwww D \\\\o \ \\\\\ \\!\\ N\\\\ 3 \\\\\ oooo o oooo o ooooo ooooo oooo)o ooooo OOOO@ @@@@ @@@@ @ @@@@@ g D OOOC)O OC)OC)\ @@@@@ @ro@@@ @oo@@ o OOOOO \\\\ \\\\ \\!!\ !\\\\ \\\vrel vr ur ur () () tl wwww@ o ! .aN5.Sr !\\\ \\\\\ \\\\\ \\\!\ tu \ooo o N'.,_, o) f. NC)!U1N O\erN <) UN]O\UI \ ) OUO6O 5O9Ob !urNO NO!hN O\ulc)! vrNO\r^ u o OhOUT O foeo ObOhO UO9Oq OUOOq Ot^OSO !. t 5 ! ! a o J6 A* F:-'< J o 60 3 l rz- > @ r l o:o a p ,^ o ; i oooc)c) oc)o<)c) oc)c)c)() =- NNJCJC) c)N<)N-.r oNoN-r NNONA a @oc)(lo b>Rx5 Vse€ J ; I o 3 ._. o to'> ()c)o()<) o-_'o" ooo()() c)<)<)c)o o NNNN--T ..7 @ONOA !()NO! x,$ O o-roo) @NONO f, . : € -f € .l iro @;!54 ()o@oN o;i(no_j € a!@:: r(roo@ !N@;! _.: o) o):: <- ooo<)o o@()L:s -13 g (o + tsONNN o-ilo\ .-E <- !o-l o : 3 --l ooc)c)c) (fooo<) o()<)oc) ()oooc) cJ c) c) () c) ()c)cJC)o oT <)<)rOO -E ?@F : g.: q6>=o> o u6> n OrzrU oa5@o @@ii@@ ,-i o) o) o) o ZT,: !!bj-- too()@ !o!@ij . i@o)N@ A-: I= noo@vl X NO!O @o@No NNNNN NNNNN NNNNN '04*A'3 NNNNN NNNNN NNNNN NNNNN I r1 NJ= @oa;o(n ajiNoo !rod@ *'N50 9E+--EAr I p3 o)NNoo l!oo5 @@@NS !T @!c)@o oc)@N! o)N@@@ NE,X : >1'X rD n \.',: - o n_us,x^: 3 r: --{x X NNNNN NNNNN NNNNN NNNNN NNNNN NNNNN NNNNN NNNNN oc)ooo oc)<><)o o; rrr lxJlr, .-v v(o !ui.i{ie oooo oooo o) ooooo r!waaw ooooo ooooo ooooo oooo) o) ooooo \\\\ \\!\ wwww@ \ \\\\\ \!\\\ - \\\\ o ooooo \\\\\ \\\\\ \\\\ \!\\! -l \ \\\\ ooooo ooooo ooooo oooo o1 ooooo @ @a@a@ @@@@@ @@@@@ @@@@@ o ooo() O \\\\! \\\!\ @@@@ @ @a@@o a O \ \\!!! \\\\\ - <) ! wwawa 3 ! \\\! \\\! \ \ \\\!\ \!\!\ \\\\! \\\\! n !oo60 \\\! \!\!! qNO\ NC)\Ul 0 l N o\vr Nc) \vrNc)\ ulN)c)!ul NO\ur N o!urc) o- O9Ou O UOUIO OUO6O 9OUOU OulOqC) UTOU'OUT -1 i OUlOC) c) ur c) \rr () ! g. o t/f o 3= fr c) c) () c) ()c)c)c>o o()o()o ooooc) oc)o<) -t -s fl N:_q,_ r-EAr H5+t 19;p ruo,; > +:; Q a.51-o U 6_osB i-T>-:Jx^rD .-v ot6 ' , !uiiUn ooooo oo)ooo ooooo wwu@w wwaaw D \\!\\ \\\\\ \!\\! \\!\\ \\\\\ 3 m !\\\\ NNNNN NNQOO 6- urvlqvtvl 9qOOO 15 ww@ww o AA}5A n m \\!\! \!\\\ \\!\\ f. l \\ooo SAAAW NO\qN C)\U1NO !urN()\ oe<)qo e()(^o(n t. sx ! J aD o JO o ,dn<: 60 o 3 3 P o ooc)c)() ()oc)(>(5 ]=: 1 oc)o() .. A€ - €:' /-l a o c ! 9-6 0 .^T )s c)ooAA oi )= € NNNNN NruNNru Nil@{; Nxa = I o o'> -' !!o5N o I O @ oo@oN o)6@N_! @@Nl@ <) ! o o @ ! @ € € € c)c)()c>o p 6- : (o o q 3 (n-'@i;i 3 ocl()'rc) 3 --l oooo "o 99x !@@!! GooiiG "' i: '' r; ! z6; I =co> :.P !!oo-V1 @> i Ou,9 sru$ru$ ZT: ONNNN NNNNN 3--l v @vr trvv X i-l oc)c)()() X :ooso aSoo!@ !-- : NON@N : l1 f A,_ N'J lD^' @o@!o 3 .: '-' 95+--!9r a I ^ ; :rl rc _a a. e'> l o p O a )ix<= : 6 € € jii^i96$ NN .]*\ € x36d; o)N!;;x .,3 <^- p (o p jloss .-.i 3= :!o! : f --l (J()O<)() .^.Pz= O .I N N N NNNN I T z6; ;I il*<=o> i 9se OANSO nV noo@Vr X vv c') q N oT NC)NO c) o;eoF ! NA.!N NNNNN NNNNN J"! r1 J P -: a;N@o olo; i;aiooo '-s K- XoX --{ : aTO 9fi+ r1' !1 1p NE,X I xr+xu a)J.. -! d s 6g$,P--lx ; c)(fc)oc) -l;- i-J>o ;;sc-.r oro , ooooo ooooo oooo6 ww@ww wwww@ p -r! \\!\\ \\\\! \\\!\ \\!\! 3 o OOOOO \\\\\ \\\\\ 6 NUNNN NNOQO o - uul()o() H ! wwwww o 3 SIAAA ft \!\!! \!\\! \!!!! \\ooq 5554a f0 NO!uN O!urNC) !urNO! =. I 9OqOU ouc)uc) uO9Oh g, n f ! ! g @ rc lO o n -l€l oo o 3 3 - o oo()()c) oT o:o=tzN u l SNNN ! !!@NN a a a ) a c)ooocl V*F a I _a rc D'> i. ooooo a o p O 6 @ 'o ooinS 'l o c)!o@o : € € E :i9 =- p @- s iooio ! o.. i;;; -i :l-nN^- 3 --.1 E ?'oo P (Y.: V)@>=oo> P !!oo- - Or,tr9z-: A=, noo@vl ^-: X i-l X N- fl A'* /o^'N'J o-: n-EA) 95+ 1? pp N!,X >f x |o Q ii 6gsB^51-o ::1 x^rD ir.rP>+ .ror5' ' FiSOn -!-l - 3' 9E f! o' n o g o J ul o -rJ l - O:O=zN 9 'rD N3Nh o_ trJ Vqi - I\ PJ f, e'> o O rD @ O g, Y a o_ qJ € € rl AJ, NQ=l € m o_= - trr+ N g>_ ::iqr N|oX :5f,:: n n XxE^-*D E i:E i-Ha il 9:1 i' !u-- Sample ID South NAD83 Z9 North NAD83 Z9 Cu PPM Ag PPM Fe % Pb PPM 1 347,150 6,376,925 235 0.2 5.22 19 2 347,175 6,376,925 186 0.2 5.38 27 3 347,200 6,376,925 186 0.2 5.44 23 4 347,225 6,376,925 171 (0.2) 5.41 33 5 347,250 6,376,925 191 (0.2) 5.14 16 6 347,275 6,376,925 95 0.2 4.33 10 7 347,300 6,376,925 82 (0.2) 5.16 12 8 347,325 6,376,925 105 (0.2) 5.04 10 9 347,350 6,376,925 106 (0.2) 4.88 9 10 347,375 6,376,925 138 (0.2) 4.46 5 11 347,400 6,376,925 123 (0.2) 4.48 9 12 347,425 6,376,925 181 (0.2) 5.53 11 13 347,450 6,376,925 191 (0.2) 5.89 8 14 347,475 6,376,925 83 (0.2) 4.79 8 15 347,500 6,376,925 255 (0.2) 7.46 17 16 347,525 6,376,925 93 0.2 4.00 13 17 347,550 6,376,925 110 0.3 4.89 14 18 347,575 6,376,925 83 0.3 3.99 16 19 347,600 6,376,925 97 (0.2) 4.49 13 20 347,625 6,376,925 131 0.2 5.31 16 21 347,650 6,376,925 257 0.2 6.28 16 22 347,675 6,376,925 427 (0.2) 9.10 21 23 347,700 6,376,925 835 0.5 12.20 22 24 347,725 6,376,925 422 1.2 7.46 17 25 347,150 6,376,950 177 (0.2) 5.72 26 26 347,175 6,376,950 443 0.2 6.81 198 27 347,200 6,376,950 238 (0.2) 6.38 17 28 347,225 6,376,950 279 0.2 5.72 18 29 347,250 6,376,950 123 0.4 4.23 11 30 347,275 6,376,950 107 0.2 4.53 14 31 347,300 6,376,950 94 (0.2) 4.56 11 32 347,325 6,376,950 48 0.2 3.24 10 33 347,350 6,376,950 117 0.2 4.16 10 34 347,375 6,376,950 180 0.2 5.88 10 35 347,400 6,376,950 144 (0.2) 5.56 13 36 347,425 6,376,950 79 (0.2) 4.59 9 37 347,450 6,376,950 197 (0.2) 6.07 14 38 347,475 6,376,950 289 (0.2) 6.92 23 39 347,500 6,376,950 159 0.2 5.52 17 40 347,525 6,376,950 112 (0.2) 4.52 9 41 347,550 6,376,950 379 0.3 7.66 27 42 347,575 6,376,950 417 0.4 8.10 25 43 347,600 6,376,950 313 0.2 6.88 17 44 347,625 6,376,950 226 0.2 5.78 19 45 347,650 6,376,950 371 0.4 6.62 21 46 347,675 6,376,950 1,115 0.5 9.36 36 47 347,700 6,376,950 515 0.3 11.30 14 48 347,150 6,376,975 137 0.3 4.65 29 49 347,175 6,376,975 128 0.3 4.33 19 50 347,200 6,376,975 213 (0.2) 5.59 23 51 347,225 6,376,975 145 (0.2) 5.36 18 52 347,250 6,376,975 131 0.2 5.16 16 53 347,275 6,376,975 131 (0.2) 5.43 14 54 347,300 6,376,975 96 0.3 3.48 16 55 347,325 6,376,975 63 0.4 3.90 11 56 347,350 6,376,975 91 0.4 4.02 13 57 347,375 6,376,975 79 (0.2) 4.05 6 58 347,400 6,376,975 75 (0.2) 3.64 14 59 347,425 6,376,975 272 0.2 5.69 43 60 347,450 6,376,975 298 0.2 7.04 22 61 347,475 6,376,975 225 0.2 5.49 10 62 347,500 6,376,975 238 0.3 6.16 22 63 347,525 6,376,975 309 (0.2) 7.43 26 64 347,550 6,376,975 145 0.3 4.48 16 65 347,575 6,376,975 261 0.2 6.38 14 66 347,600 6,376,975 490 0.3 8.44 14 67 347,625 6,376,975 466 0.3 8.73 17 68 347,650 6,376,975 479 0.5 7.23 25 69 347,675 6,376,975 878 0.4 8.88 30 70 347,700 6,376,975 417 0.4 9.52 12 71 347,725 6,376,975 703 0.2 12.75 12 72 347,150 6,377,000 180 0.4 5.30 30 73 347,175 6,377,000 156 (0.2) 4.56 32 74 347,200 6,377,000 139 (0.2) 4.75 23 75 347,225 6,377,000 126 0.2 4.80 19 76 347,250 6,377,000 71 (0.2) 3.68 10 77 347,275 6,377,000 115 (0.2) 4.49 7 78 347,300 6,377,000 81 0.2 4.85 24 79 347,325 6,377,000 88 0.3 4.86 16 80 347,350 6,377,000 194 (0.2) 6.14 28 81 347,375 6,377,000 126 (0.2) 4.62 8 82 347,400 6,377,000 117 0.2 4.99 9 83 347,425 6,377,000 209 (0.2) 6.17 19 84 347,450 6,377,025 323 (0.2) 7.00 33 85 347,475 6,377,025 239 0.2 6.84 56 86 347,500 6,377,025 242 (0.2) 5.60 15 87 347,525 6,377,025 483 0.2 8.54 34 88 347,550 6,377,025 274 0.2 6.61 31 89 347,575 6,377,025 294 0.2 6.67 29 90 347,600 6,377,025 176 (0.2) 5.98 16 91 347,625 6,377,025 242 (0.2) 6.05 11 92 347,650 6,377,025 300 (0.2) 6.16 99 93 347,675 6,377,025 180 0.2 5.87 9 94 347,700 6,377,025 598 0.3 13.70 11 95 347,725 6,377,025 851 0.5 14.30 69