Vancouver, British Columbia–(Newsfile Corp. – May 5, 2022) – Goldshore Resources Inc. (TSXV: GSHR) (OTCQB: GSHRF) (FSE: 8X00) (“Goldshore” or the “Company“), is pleased to announce assay results in hole MQD-22-014 from its ongoing 100,000-meter drill program at the Moss Lake Project in Northwest Ontario, Canada. Drilling is aiming to better define and expand high-grade structural zones within the Moss Lake deposit to improve the overall grade and volume beyond that of the historic mineral resource.
- Broad zone of high-grade mineralization confirming the tenor of mineralization modeled in the QES Zone with best intercepts of:
- 128.3m at 1.05 g/t Au from 121.3m, including
- 40.6m at 1.99 g/t Au from 139.4m,
- 3.6m at 1.80 g/t Au from 199.0m, and
- 22.0m at 1.25 g/t Au from 227.0m.
- New high grade gold mineralization open in all directions with visible gold intersected in a northern parallel structure. This northern structure is interpreted to be the same parallel structure intersected over 100 metres further to the east (see press release dated January 28, 2022). In addition, the identification of VG in this northern structure could provide elevated milling recoveries in any future operation. The drilling returned:
- 16.0m at 5.31 g/t Au from 477.0m, including
- 5.25m at 15.8 g/t Au from 477.75m
- Expanding Drill Capacity through the engagement of two additional drill contractors who are mobilizing three rigs to site in the coming week. This will enable Goldshore to increase the drilling rate at the Moss Lake gold deposit and expand the drill program to the Coldstream area to evaluate the gold deposit at East Coldstream and copper-gold-cobalt mineralization at North Coldstream.
Brett Richards, President and Chief Executive Officer of Goldshore, commented: “The drilling intercept of 128.3m at 1.05 g/t Au reaffirms our view that the Moss Lake gold project contains a significant volume of +1 g/t Au mineralization that can underpin a meaningful, economic gold deposit. The fact that we are continuing to intersect gold mineralization outside of the volume modelled in 2013 also affirms our belief that the deposit is significantly larger than previously interpreted. Separately, we are pleased to be bringing in additional drill contractors that will enable us to increase our drilling rate at Moss Lake while commencing drilling at Coldstream.”
Figure 1 and Table 1 summarize the significant intercepts in MQD-22-014. Figure 2 shows the visible gold seen at 478.1 meters depth, which corresponds to the high-grade parallel structure. Figure 3 and Table 2 show the drill hole location.
Figure 2: Visible gold in quartz-pyrite veins at 478.1m in MQD-22-014
Table 1: Significant downhole gold intercepts in MQD-22-014
|HOLE ID||FROM||TO||HOLE LENGTH (m)||TRUE WIDTH
|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. Shaded 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|
MQD-22-014 was drilled 120 meters west of MQD-21-009 (see press release dated January 28, 2022) at a -45° dip and 335° azimuth to test the 2013 resource model and twin the historic hole 90-203.
The reported significant intercept of 128.3m at 1.05 g/t Au from 121.3m occurs within a broader zone of strongly silica-sericite-chlorite±carbonate altered diorite that assays 200.75m at 0.77 g/t Au from 14m above a 0.3 g/t Au cutoff. The better grade segments (e.g., 40.6m at 1.99 g/t Au from 139.4m) are characterized by intense foliation and brecciation, which reflect numerous sigmoidal shear zones that provide the plumbing for the hydrothermal system.
These results are similar to those intersected in the historic hole, which returned 136.0m at 1.09 g/t Au from 137.0m.
Importantly, we continue to intersect parallel structures that were not previously reported. Visible gold was intersected within a 1.45-meter-wide quartz-pyrite-chalcopyrite vein from 477.75-479.20m, which averages 54.1 g/t Au. This occurs within a biotite-altered diorite that returned 16.0m at 5.31 g/t Au from 477.0m.
Peter Flindell, VP Exploration, commented: “These drilling results confirm the historic drill results and help us to understand the non-linear distribution of high grades that will enable us to model the higher-grade gold resource more accurately later in the year. Our relogging work and surveying of historic drill collars will also allow us to incorporate many of the historic drillholes, which will reduce the number of holes we need to drill in this campaign. Just as we are intersecting new parallel zones of mineralization that will expand the Mineral Resource, we are also identifying mineralization in the historic holes that was previously unsampled, thereby adding assay data to our database.”
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. is currently a strategic shareholder of Goldshore with an approximate 22% 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.
Moss Lake 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 was completed on Moss Lake in 2013 and published by Moss Lake Gold1. A historical mineral resource estimate was completed on the East Coldstream Deposit in 2011 by Foundation Resources Inc2,3. 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 Gold Mines Ltd. (“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 Deposit1 (2013 resource 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 Deposit2 (2011 resource estimate)|
|East Coldstream Total||3,516,700||0.85||96,400||30,533,000||0.78||763,276|
(1) Source: Poirier, S., Patrick, G.A., Richard, P.L., and Palich, J., 2013. Technical Report and Preliminary Economic Assessment for the Moss Lake Project, 43-101 technical report prepared for Moss Lake Gold Mines Ltd. Moss Lake Deposit resource estimate is based on 0.5 g/t Au cut-off grade for open pit and 2.0 g/t Au cut-off grade for underground resources.
(2) Source: McCracken, T., 2011. Technical Report and Resource Estimate on the Osmani Gold Deposit, Coldstream Property, Northwestern Ontario, 43-101 technical report prepared for Foundation Resources Inc. and Alto Ventures Ltd. East Coldstream Deposit resource estimate is based on a 0.4 g/t Au cut-off grade.
(3) The reader is cautioned that the above referenced “historical mineral resource” estimates are considered historical in nature and as such is based on prior data and reports prepared by previous property owners. A qualified person has not done sufficient work to classify the historical estimates as current resources and Goldshore is not treating the historical estimates as current resources. Significant data compilation, re-drilling, re-sampling and data verification may be required by a qualified person before the historical estimate on the Moss Lake Gold Project can be classified as a current resource. There can be no assurance that any of the historical mineral resources, in whole or in part, will ever become economically viable. In addition, mineral resources are not mineral reserves and do not have demonstrated economic viability. Even if classified as a current resource, there is no certainty as to whether further exploration will result in any inferred mineral resources being upgraded to an indicated or measured mineral resource category.
Table 4: Reported Historical Production from the North Coldstream Deposit4
|Deposit||Tonnes||Cu %||Au g/t||Ag||Cu lbs||Au oz||Ag oz|
(4) Source: Schlanka, R., 1969. Copper, Nickel, Lead and Zinc Deposits of Ontario, Mineral Resources Circular No. 12, Ontario Geological Survey, pp. 314-316.
Peter Flindell, 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.
P. +1 604 288 4416 M. +1 905 449 1500
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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.
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