
Goldshore Resources Inc. (TSX-V: GSHR) (OTCQB: GSHRF) (FWB: 8X00) is pleased to announce assay results from its ongoing 100,000-meter drill program at the Moss Lake Project in Northwest Ontario, Canada.
Results for seven holes, drilled to expand the coverage of the high-grade shears in the QES Zone, have confirmed higher-grade shear-hosted gold mineralization within a large volume of well mineralized diorites. These results are all within the $1500 Whittle pit that constrains the current resource and identifies new high-grade shears. Best intercepts include:
A new parallel mineralized shear structure has been discovered 150m south of the main QES system containing high grade mineralization within a sheared intermediate volcanic package with best intercepts of:
President and CEO Brett Richards stated: “The results from these drill holes in the QES Zone are part of a 52-hole data set that was not included in the recent mineral resource estimate. They confirm our belief that there are additional high-grade shear zones within the deposit that will potentially add to the shear domain component of the mineral resource that we anticipate will be prioritized in the mining schedule when we move towards conducting a preliminary economic analysis next year.”
Figure 1 shows the better intercepts in plain view and Figure 2 is a typical section through hole MQD-22-087. Table 1 shows the significant intercepts. Table 2 shows the drill hole locations.
Figure 1: Drill plan showing best of several +1 g/t Au intercepts relative to shear and intrusion domains
Figure 2: Drill section through MQD-22-0087 relative to shear and intrusion domains
Results have been received for six holes that have infilled areas of the QES Zone that are between sections drilled by historic holes with collar survey problems. As a result, they will replace the low-confidence historic holes in the upcoming resource model update.
A seventh hole was drilled to the southeast of the QES Zone to investigate two historical showing along a parallel structure of the QES Zone but did not intersect significant mineralization.
As with the historic holes, these holes intersected several broad zones of low-grade mineralization within the altered diorite intrusion host. Examples include 0.77 g/t Au over 83m from 493m depth in MQD-22-075; 0.41 g/t Au over 32.45m from 437.55m and 0.71 g/t Au over 131.1m from 493m in MQD-22-076; 0.54 g/t Au over 102m from 476m and 0.39 g/t Au over 27.95m from 643m in MQD-22-080; 0.78 g/t Au over 70m from 419m and 0.50 g/t Au over 28.75m from 521.25m in MQD-22-085; 0.50 g/t Au over 115.9m from 408.1m in MQD-22-087; and 0.48 g/t Au over 27.45m from 552.05m in MQD-22-090A.
All these low-grade zones occur as envelopes to higher-grade structures that form a three-dimensional, anastomosing shear network that has developed in response to strain on the altered diorite intrusion. Results include the broad zones of +1 g/t Au mineralization shown in the highlights (e.g., 1.31 g/t Au over 63.6m from 427m depth in MQD-22-090A) and several narrow high-grade intervals, including 10.1 g/t Au over 0.7m from 545.8m and 36.9 g/t Au over 1m from 577m in MQD-22-076; 10.0 g/t Au over 1m from 427m in MQD-22-085; 20.6 g/t Au over 0.9m from 370.65m, 28.3 g/t Au over 0.3m from 540.3m and 11.5 g/t Au over 3.1m from 555.2m in MQD-22-087; and 19.4 g/t Au over 1.15m from 455.85m in MQD-22-090A.
An additional parallel shear was discovered within the intermediate volcanic package approximately 150m south of the main QES system which contains broad intercepts of low-grade mineralization including 0.91 g/t over 24.8m from 246.4m in MQD-22-080; 0.33 g/t over 45.7m from 150.0m in MQD-22-085; 0.42 g/t over 39.0m from 189.0m in MQD-22-087 containing internal higher grade intercepts including 3.44 g/t Au over 5.8m from 246.4m depth in MQD-22-080; 1.22 g/t Au over 4.0m from 206.0m depth in MQD-22-087; 1.15 g/t Au over 7.3m from 75.0m depth in MQD-22-090A.
Importantly, these intercepts have identified additional high-grade shears not modelled in the recent Mineral Resource.
Pete Flindell, VP Exploration for Goldshore, said “These drill results confirm high-grade shears that we have modelled at the QES Zone and confirmed additional shears that we expect to include in the next mineral resource update early next year.”
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Notes:
(1) The Moss Lake Deposit hosts an estimated inferred mineral resource of 4.17Moz Au (see Goldshore’s news release dated November 15, 2022). A technical report is being prepared in accordance with NI 43-101 and will be available on the Company’s website and SEDAR within 45 days of November 15, 2022.
Notes:
(2) Source: McCracken, T. “Technical Report and Resource Estimate on the Osmani Gold Deposit, Coldstream Property, Northwestern Ontario”, prepared for Foundation Resources Inc. and Alto Ventures Ltd. The East Coldstream Historical Estimate is based on a 0.4 g/t Au cut-off grade. The qualified persons for the East Coldstream Historical Estimate are Todd McCracken, P.Geo. (Tetratech Wardrop), and Jeff Wilson, Ph.D., P.Geo. (Tetratech Wardrop), and the effective date of the East Coldstream Historical Estimate is December 12, 2011. Resources are presented unconstrained, undiluted and in situ. The East Coldstream Historical Estimate includes 2 gold-bearing zones. A cut-off grade of 0.4 g/t Au was selected as the official resource cut-off grade. The East Coldstream Historical Estimate is based on 116 diamond drill holes drilled from 1986 to 2011. A fixed density of 2.78 g/cm3 was used. Capping was established at 5.89 g/t Au and 5.70 g/t Au for domains EC-1 and EC-2, respectively. This is supported by statistical analysis and the high grade distribution within the deposit. Compositing was done on drill hole sections falling within the mineralized zone solids (composite = 1 m). Resources were evaluated from drill hole samples using the ID2 interpolation method in a multi-folder percent block model using Datamine Studio 3 version 3.20.5321.0. Resource categorization is based on spatial continuity based from the variography of the assays within the drillholes. Ounce (troy) = metric tons x grade / 31.10348. Calculations used metric units (metres, tonnes and g/t). The number of metric tonnes was rounded to the nearest thousand. Any discrepancies in the totals are due to rounding effects; rounding followed the recommendations in NI 43-101.
(3) The reader is cautioned that the East Coldstream Historical Estimate is considered historical in nature and as such is based on prior data and reports prepared by previous property owners. The reader is cautioned not to treat it, or any part of it, as current mineral resources or reserves. The Company has determined this historical resource is reliable, and relevant to be included here in that it demonstrates simply the mineral potential of the Moss Lake Gold Project. A qualified person has not done sufficient work to classify the East Coldstream Historical Estimate as a current resource and Goldshore is not treating the East Coldstream Historical Estimate as a current resource. Significant data compilation, re-drilling, re-sampling and data verification may be required by a qualified person before the East Coldstream Historical Estimate 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. The East Coldstream Historical Estimate relating to inferred mineral resources was calculated using prior mining industry standard definitions and practices for estimating mineral resource and mineral reserves. Such prior definitions and practices were utilized prior to the implementation of the current standards of the Canadian Institute of Mining for mineral resource estimation, and have a lower level of confidence.
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