Vancouver, British Columbia–(Newsfile Corp. – September 12, 2022) – Goldshore Resources Inc. (TSXV: GSHR) (OTCQB: GSHRF) (FSE: 8X00) (“Goldshore” or the “Company“), is pleased to announce assay results from eight holes drilled to test gold mineralization at the East Coldstream deposit at the Moss Lake Project in Northwest Ontario, Canada (the “Moss Lake Gold Project“).
President and CEO Brett Richards stated: “These first results are extremely encouraging and significant to the overarching strategy of developing a secondary resource to Moss Lake. This will provide optionality that can only help improve the new PEA study next year. The results also point to a second significant project within our land package, which highlights the potential for further discoveries.”
Figure 1 shows the location of the East Coldstream deposit relative to the Moss Lake deposit and the Archean Shebandowan Greenstone Belt. Table 1 and Figure 3 show the significant intercepts. Table 2 and Figure 2 show the drill hole locations. Figures 4 and 5 show a cross section through CED-22-006 and long section along the southern zone, respectively.
Figure 1: Location map showing East Coldstream relative to Moss Lake
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Figure 2: Drill plan showing drill holes (long section is Figure 5)
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Figure 3: Drill plan showing best of several +1 g/t Au intercepts
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Figure 4: Drill section through CED-22-006 and the Main Lens
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Figure 5: Long section through the Main and Sanders Lenses
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Table 1: Significant downhole gold intercepts
|CED-22-002||No significant assays|
|Intersections calculated above a 0.3 g/t Au cut off with a top cut of 30 g/t Au and a maximum internal waste interval of 10 metres. Bordered intervals are intersections calculated above a 1.0 g/t Au cut off. Intervals in bold are those with a grade thickness factor exceeding 20 gram x metres / tonne gold. True widths are approximate and assume a subvertical body.|
Table 2: Location of drill holes in this press release
|Approximate collar coordinates in NAD 83, Zone 15N|
Results have been received for eight of the initial 17 holes in the first pass drilling program at East Coldstream. These drillholes tested the existing mineralized lenses, as well as possible eastern and down-dip extensions.
Our work on the mineralization paragenesis and its structural controls has shown that gold mineralization is related to pervasive silica-hematite alteration and sulfide veining associated with an extensional brecciation event following extensive shearing. At the deposit scale, this formed three lenticular bodies within two main shear zones (Figure 1). Based on structural measurements from oriented core, each body has a steeply west-dipping plunge and a gently east-pitching stretching lineation that creates an internal fabric to mineralization (Figure 4). This structural control creates the potential for additional high-grade mineralization to occur below the shallowly drilled portions of the shears zones such as encountered in CED-22-007.
CED-22-001 and -002 tested a similar geophysical feature to the east of the East Coldstream deposit. CED-22-001 was drilled closest to East Coldstream and encountered narrow zones of mineralization, while CED-22-002 was drilled 300 meters further east and did not encounter significant results. This sterilizes the immediate extension, but given the lenticular geometry of mineralization, leaves open the prospectively of the structure further to the east.
CED-22-003 and -004 drilled the North and Main Lenses, respectively. Both holes intersected broad low-grade mineralized zones, including 19.15m @ 0.61 g/t Au from 269.55m in CED-22-003; and 48m @ 0.39 g/t Au from 168m and 23m @ 1.34 g/t Au in CED-22-004.
Holes CED-22-005 to -008 tested down plunge extensions of the known mineralization. All holes intersected variable widths of higher grade mineralization, including 17.3m @ 1.55 g/t Au from 487m in CED-22-005; 20.0m @ 1.15 g/t Au from 402m, 26.0m @ 1.66 g/t Au from 451m, and 25.7m @ 2.07 g/t Au from 488m in CED-22-006; 37.05m @ 1.54 g/t Au from 209.3m in CED-22-007; and 27.9m @ 1.14 g/t Au from 387m in CED-22-008.
Pete Flindell, VP Exploration for Goldshore, said “Our analysis of drill results at East Coldstream confirms the two parallel shear zones that were modelled in the past. The recognition of a greater structural control within these shears has led to the modelling of three steeply dipping lenticular shoots that remain open at depth. A gently dipping internal fabric suggests that mineralization is focused within discrete structures that may allow us to model a higher-grade resource than exists in the historic estimate.”
Analytical and QA/QC Procedures
All samples were sent to ALS Geochemistry in Thunder Bay for preparation and analysis was performed in the ALS Vancouver analytical facility. ALS is accredited by the Standards Council of Canada (SCC) for the Accreditation of Mineral Analysis Testing Laboratories and CAN-P-4E ISO/IEC 17025. Samples were analyzed for gold via fire assay with an AA finish (“Au-AA23”) and 48 pathfinder elements via ICP-MS after four-acid digestion (“ME-MS61”). Samples that assayed over 10 ppm Au were re-run via fire assay with a gravimetric finish (“Au-GRA21”).
In addition to ALS quality assurance / quality control (“QA/QC”) protocols, Goldshore has implemented a quality control program for all samples collected through the drilling program. The quality control program was designed by a qualified and independent third party, with a focus on the quality of analytical results for gold. Analytical results are received, imported to our secure on-line database and evaluated to meet our established guidelines to ensure that all sample batches pass industry best practice for analytical quality control. Certified reference materials are considered acceptable if values returned are within three standard deviations of the certified value reported by the manufacture of the material. In addition to the certified reference material, certified blank material is included in the sample stream to monitor contamination during sample preparation. Blank material results are assessed based on the returned gold result being less than ten times the quoted lower detection limit of the analytical method. The results of the on-going analytical quality control program are evaluated and reported to Goldshore by Orix Geoscience Inc.
Goldshore is an emerging junior gold development company, and owns the Moss Lake Gold Project located in Ontario. Wesdome Gold Mines Ltd. (“Wesdome“), is currently a large shareholder of Goldshore with an approximate 27% equity position in the Company. Well-financed and supported by an industry-leading management group, board of directors and advisory board, Goldshore is positioned to advance the Moss Lake Gold Project through the next stages of exploration and development.
About the Moss Lake Gold Project
The Moss Lake Gold Project is located approximately 100 km west of the city of Thunder Bay, Ontario. It is accessed via Highway 11 which passes within 1 km of the property boundary to the north. The Moss Lake Gold Project covers 14,292 hectares and consists of 282 unpatented and patented mining claims.
The Moss Lake Gold Project hosts a number of gold and base metal rich deposits including the Moss Lake Deposit, the East Coldstream Deposit (Table 3), the historically producing North Coldstream Mine (Table 4), and the Hamlin Zone, all of which occur over a mineralized trend exceeding 20 km in length. A historical preliminary economic assessment (the “Moss Lake Historical Estimate“) was completed on the Moss Lake Gold Project in 2013 and published by Moss Lake Gold Mines Ltd. (“Moss Lake Gold Mines“)1,3. A historical mineral resource estimate (the “East Coldstream Historical Estimate“) was completed on the East Coldstream Deposit in 2011 by Foundation Resources Inc.2,3 In addition to these zones, the Moss Lake Gold Project also hosts a number of under-explored mineral occurrences which are reported to exist both at surface and in historically drilled holes. The Moss Lake Deposit is a shear-hosted disseminated-style gold deposit which outcrops at surface. It has been drilled over a 2.5 km length and to depths of 300 m with 376 holes completed between 1983 and 2017. The last drilling program conducted in 2016 and 2017 by Wesdome, which consisted of widely spaced holes along the strike extension of the deposit was successful in expanding the mineralized footprint and hydrothermal system 1.6 km to the northeast. Additionally, the deposit remains largely open to depth. In 2017, Wesdome completed an induced polarization survey which traced the potential extensions of pyrite mineralization associated with the Moss Lake Deposit over a total strike length of 8 km and spanning the entire extent of the survey grids.
The East Coldstream Deposit is a shear-hosted disseminated-style gold deposit which locally outcrops at surface. It has been drilled over a 1.3 km length and to depths of 200 m with 138 holes completed between 1988 and 2017. The deposit remains largely open at depth and may have the potential for expansion along strike. Historic drill hole highlights from the East Coldstream Deposit include 4.86 g/t Au over 27.3 m in C-10-15.
The historically producing North Coldstream Mine is reported to have produced significant amounts of copper, gold and silver4 from mineralization with potential iron-oxide-copper-gold deposit style affinity. The exploration potential immediately surrounding the historic mining area is not currently well understood and historic data compilation is required.
The Hamlin Zone is a significant occurrence of copper and gold mineralization, and also of potential iron-oxide-copper-gold deposit style affinity. Between 2008 and 2011, Glencore tested Hamlin with 24 drill holes which successfully outlined a broad and intermittently mineralized zone over a strike length of 900 m. Historic drill hole highlights from the Hamlin Zone include 0.9 g/t Au and 0.35% Cu over 150.7 m in HAM-11-75.
The Moss Lake, East Coldstream and North Coldstream deposits sit on a mineral trend marked by a regionally significant deformation zone locally referred to as the Wawiag Fault Zone in the area of the Moss Lake Deposit. This deformation zone occurs over a length of approximately 20 km on the Moss Lake Gold Project and there is an area spanning approximately 7 km between the Moss Lake and East Coldstream deposits that is significantly underexplored.
Table 3: Historical Mineral Resources1,2,3
|Deposit||Tonnes||Au g/t||Au oz||Tonnes||Au g/t||Au oz|
|Moss Lake Historical Estimate|
|Open Pit Potential||39,795,000||1.1||1,377,300||48,904,000||1.0||1,616,300|
|Moss Lake Total||39,795,000||1.1||1,377,300||50,364,000||1.1||1,751,600|
|East Coldstream Historical Estimate|
|East Coldstream Total||3,516,700||0.85||96,400||30,533,000||0.78||763,276|
Table 4: Reported Historical Production from the North Coldstream Deposit4
|Deposit||Tonnes||Cu %||Au g/t||Ag||Cu lbs||Au oz||Ag oz|
Peter Flindell, P.Geo., MAusIMM, MAIG, Vice President – Exploration of the Company, a qualified person under NI 43-101 has approved the scientific and technical information contained in this news release.
Neither the TSXV nor its Regulation Services Provider (as that term is defined in the policies of the TSXV) accepts responsibility for the adequacy or accuracy of this release.
For More Information – Please Contact:
Brett A. Richards
President, Chief Executive Officer and Director
Goldshore Resources Inc.
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Cautionary Note Regarding Forward-Looking Statements
This news release contains statements that constitute “forward-looking statements.” Such forward-looking statements involve known and unknown risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words “expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,” “projects,” “potential” and similar expressions, or that events or conditions “will,” “would,” “may,” “could” or “should” occur.
Forward-looking statements in this news release include, among others, statements relating to expectations regarding the exploration and development of the Moss Lake Gold Project, and other statements that are not historical facts. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors and risks include, among others: the Company may require additional financing from time to time in order to continue its operations which may not be available when needed or on acceptable terms and conditions acceptable; compliance with extensive government regulation; domestic and foreign laws and regulations could adversely affect the Company’s business and results of operations; the stock markets have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely affect the price of the Company’s securities, regardless of its operating performance; and the impact of COVID-19.
The forward-looking information contained in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event that management’s beliefs, estimates or opinions, or other factors, should change.
This news release does not constitute an offer to sell, or a solicitation of an offer to buy, any securities in the United States. The securities have not been and will not be registered under the United States Securities Act of 1933, as amended (the “U.S. Securities Act”) or any state securities laws and may not be offered or sold within the United States or to U.S. Persons unless registered under the U.S. Securities Act and applicable state securities laws or an exemption from such registration is available.