Magnum Goldcorp Intersects Multiple High Grade Gold Intervals, Including 3.47 M of 13.90 G/t and 9.30 M of 4.51 G/t
Magnum Goldcorp Intersects Multiple High Grade Gold Intervals, Including 3.47 M of 13.90 G/t and 9.30 M of 4.51 G/t
West Vancouver, British Columbia--(Newsfile Corp. - August 16, 2022) - Magnum Goldcorp Inc. (TSXV: MGI) (the "Company" or "Magnum") is pleased to announce encouraging analytical results from the Company's recently completed helicopter-supported drill program on its gold exploration property (the "LH Property"), located near Silverton, British Columbia. The LH Property consists of 19 contiguous crown granted claims, seven mineral claims and a mineral lease located approximately 6 km south of Silverton, east of Slocan Lake.
不列顛哥倫比亞省西温哥華-(Newsfile Corp.-2022年8月16日)-Magnum Goldcorp Inc.(多倫多證券交易所股票代碼:MGI)(以下簡稱“公司”或“Magnum”)高興地宣佈,該公司最近完成的直升機輔助鑽探項目對其位於不列顛哥倫比亞省西爾弗頓附近的金礦勘探項目(“LH礦”)的分析結果令人鼓舞。該地產包括19個毗連的皇冠授權權、7個礦業權和一個位於西爾弗頓以南約6公里、斯洛坎湖以東的礦產租賃權。
"The Company considers the results of the 2022 program to be very significant. The holes completed continue to document multiple mineralized, variable gold-bearing intervals, including high-grade gold-bearing intervals defined as those above 10 g/t Au, consistent with previous programs. We are extremely encouraged by these results from the LH Property and the potential to identify an initial NI 43-101 compliant resource in the near future. We are actively working to continue our drill program on the property to realize that goal", said Douglas Mason, President & CEO of Magnum Goldcorp Inc.
Magnum Goldcorp Inc.首席執行官總裁和首席執行官道格拉斯·梅森表示:“本公司認為2022年計劃的結果非常重要。已完成的鑽孔繼續記錄了多個礦化的、可變的含金區段,包括定義為高於10 g/t Au的高品位含金區段,與以前的計劃一致。我們對LH型金礦的這些結果以及在不久的將來確定符合NI 43-101標準的初步資源的潛力感到非常鼓舞。我們正在積極努力繼續我們在該礦藏的鑽探計劃,以實現這一目標。”
The Company completed the drill program to continue evaluation of multiple high-grade, gold-bearing, pyrrhotite mineralized zones spatially associated with the LH underground workings (see News Releases dated May 30, 2022 and July 4, 2022). Gold-bearing zones have been previously documented from both underground chip sampling by a previous operator and diamond drilling by Magnum (see News Releases dated Nov. 25, 2019, Feb 8, 2018, Aug. 18, 2015).
該公司完成了鑽探計劃,以繼續評估與LH型地下工作面空間上相關的多個高品位、含金磁黃鐵礦礦化帶(見2022年5月30日和2022年7月4日的新聞稿)。以前的運營商的地下芯片採樣和Magnum的鑽石鑽探都曾記錄過含金帶(見日期為2019年11月25日、2018年2月8日、2015年8月18日的新聞稿)。
The holes completed in 2022 continue to document multiple, pyrrhotite mineralized, variably gold-bearing zones, including high-grade, gold-bearing intervals, consistent with previous programs. Very high-grade intercepts, arbitrarily defined as those above 10 g/t Au, are comparatively small, however, they are contained within much larger mineralized intervals and, when composited over the width of those intervals, return respectable average grades over encouraging widths. Furthermore, the strong correlation between prominent magnetic anomalies and well mineralized, gold-bearing intervals has been extended to both depth and farther south, beyond immediate proximity to the LH Underground workings. More specifically, shallow intercepts in both holes LH22-55 and 56 are located approximately 160 m south of the surface trace of the underground workings.
2022年完成的鑽孔繼續記錄了多個磁黃鐵礦礦化的可變含金帶,包括高品位的含金層,與以前的計劃一致。極高品位的截距,隨意定義為10g/t Au以上的截距,相對較小,然而,它們包含在更大的礦化區間內,當在這些區間的寬度上覆合時,在鼓勵的寬度上返回可觀的平均品位。此外,顯著的磁性異常與礦化良好的含金間隔之間的強烈相關性已擴展到深度和更南邊,超出了緊鄰LH型地下工作場所的範圍。更具體地説,LH22-55和56號孔中的淺層截流段位於地下工作面痕跡以南約160米處。
Cumulatively, results to date document multiple high-grade, gold-bearing intervals, varying in thickness from at least 1 metre to in excess of 8.75 m thick. Sections document mineralized zones extending to at least 100 m below surface and approximately 160 m south of the underground workings. In addition, drill hole LH86-06 (drilled previously by Noranda Exploration Ltd, internal report dated 1986) documents two mineralized intervals, the first grading 1.46 g/t over 10.65 m and the second grading 1.46 g/t over 13.20 m, with the second located 150 m below surface at the eastern end of the surface projection of the LH Underground Workings.
到目前為止,累積起來的結果證明有多個高品位的含金層段,厚度從至少1米到超過8.75米不等。各節記錄了礦化區延伸到地表以下至少100米和地下工作面以南約160米的地方。此外,LH86-06鑽孔(由Noranda Explore Ltd以前鑽探,日期為1986年的內部報告)記錄了兩個礦化區段,第一個品位為1.46克/噸,超過10.65米,第二個品位為1.46克/噸,超過13.20米,第二個品位在地表以下150米處,位於左側地下巷道地面投影的東端。
Underground sampling confirms that variable, moderate to high-grade gold (≤154.08 g/t) has been documented throughout Levels 1 and 2, from east to west (approximately 100 m) and north to south (approximately 40 m). Drilling by the Company continues to document high-grade, gold-bearing mineralization, extending to a depth of at least 100 m below surface, with previous drill-hole LH86-06 documenting mineralization extending to a depth of at least 150 m below surface at the east end of the underground workings. Taken together, these data are interpreted to indicate strong potential to delineate a mineral resource spatially associated with the LH Underground Workings.
地下采樣證實,從東到西(約154.08米)和從北到南(約40米)的整個1級和2級都記錄有可變的中高品位金(≤154.08 g/t)。本公司的鑽探繼續記錄高品位的含金礦化,並延伸到地表以下至少100米的深度,之前的LH86-06鑽孔記錄的礦化延伸到地下工作場所東端至少地表以下150米的深度。綜上所述,這些數據被解讀為具有很強的潛力,可以在空間上圈定與LH型地下開採有關的礦產資源。
Previously tested pyrrhotite-bearing mineralized zones are spatially associated with prominent magnetic signatures in the immediate vicinity of the underground workings. Gold-bearing intercepts documented from within, and adjacent to, the underground workings are strongly correlated with pyrrhotite mineralization, with the intensity of pyrrhotite mineralization strongly correlated with gold content. Therefore, high intensity magnetic anomalies are interpreted to represent potential high-grade gold-bearing zones within the mineralized system and comprised the targets for the 2022 drill program. Furthermore, additional prominent, high intensity magnetic anomalies evident in the Fingland Creek drainage are interpreted to be similarly correlated with gold-bearing pyrrhotite mineralization.
以前測試過的含磁黃鐵礦礦化帶在空間上與地下工作面附近的顯著磁性特徵有關。地下巷道內部和鄰近的含金截留與磁黃鐵礦礦化密切相關,磁黃鐵礦礦化強度與金含量密切相關。因此,高強度磁異常被解釋為代表成礦系統內潛在的高品位含金帶,並構成2022年鑽探計劃的目標。此外,在Fingland Creek排水系統中明顯的額外顯著的高強度磁異常被解釋為與含金磁黃鐵礦礦化類似。
A total of 7 diamond drill holes, totaling 1,248 m, were completed from 2 pads, one 47 m north of the underground workings, intended to test the down-dip extension of the mineralized system with depth, and the second 160 m south of the underground workings, intended to test a prominent magnetic lobe extending from a larger magnetic anomaly northwest toward the underground workings. The following table provides details of the orientations of the drill holes from each pad.
總共完成了7個鑽石鑽孔,總計1248米,從兩個墊層中完成,一個在地下工作面以北47m,旨在測試礦化系統向下延伸的深度,第二個在地下工作面以南160m,旨在測試從較大的西北向磁異常向地下工作面延伸的突出磁瓣。下表提供了每個墊片上鑽孔方向的詳細信息。
Hole | Pad | Azimuth | Inclination | Depth (m) |
LH 22-50 | 1 | 170° | -47° | 120.3 |
LH 22-51 | 1 | 170° | -70° | 90.3 |
LH 22-52 | 1 | 140° | -47° | 90.8 |
LH 22-53 | 2 | 330° | -55° | 251 |
LH 22-54 | 2 | 334° | -51° | 215.4 |
LH 22-55 | 2 | 338° | -48° | 250 |
LH 22-56 | 2 | 170° | -45° | 230.4 |
孔洞 | 襯墊 | 方位角 | 傾角 | 深度(米) |
陸兆禧22-50 | 1 | 170° | -47° | 120.3 |
路22-51 | 1 | 170° | -70° | 90.3 |
路22-52 | 1 | 140° | -47° | 90.8 |
路22-53 | 2 | 330° | -55° | 251 |
路22-54 | 2 | 334° | -51° | 215.4 |
LH22-55 | 2 | 338° | -48° | 250 |
路22-56 | 2 | 170° | -45° | 230.4 |
Visually defined high-grade pyrrhotite mineralized intervals were selected for initial analysis. The holes also include numerous low to moderate grade pyrrhotite mineralized intervals which may be analyzed at a future date. Select analytical results from the 2022 drill program are presented in the following table:
選擇目視確定的高品位磁黃鐵礦礦化區段進行初步分析。這些洞還包括許多低至中品位的磁黃鐵礦礦化區間,這些礦化區間可能會在未來的某個日期進行分析。下表列出了2022年鑽探計劃的部分分析結果:
Drill Hole | From (m) | To (m) | Width (m) | Au (g/t) | Ag (g/t) |
LH-22-53 | 34.57 | 41.40 | 6.83 | 1.60 | 0.43 |
includes | 40.50 | 41.40 | 0.90 | 5.35 | 1.19 |
LH22-55 | 12.59 | 14.16 | 1.57 | 15.92 | 1.93 |
26.84 | 27.88 | 1.04 | 2.38 | 0.64 | |
230.31 | 244.10 | 13.79 | 0.67 | 0.30 | |
includes | 230.31 | 231.40 | 1.09 | 3.23 | 0.62 |
includes | 234.95 | 236.00 | 1.05 | 1.05 | 0.38 |
LH22-56 | 11.28 | 14.75 | 3.47 | 13.90 | 1.53 |
includes | 11.66 | 13.26 | 1.60 | 19.31 | 2.27 |
20.40 | 21.83 | 1.43 | 2.81 | 0.93 | |
includes | 20.76 | 21.07 | 0.31 | 10.60 | 3.57 |
27.28 | 28.95 | 1.67 | 3.01 | 0.47 | |
215.50 | 224.80 | 9.30 | 4.51 | 0.72 | |
includes | 215.50 | 216.13 | 0.63 | 1.87 | 1.18 |
includes | 222.22 | 223.36 | 1.14 | 32.00 | 3.54 |
鑽孔 | 發件人(M) | 至(M) | 寬度(米) | Au(克/噸) | 銀(克/噸) |
LH-22-53 | 34.57 | 41.40 | 6.83 | 1.60 | 0.43 |
包括 | 40.50 | 41.40 | 0.90 | 5.35 | 1.19 |
LH22-55 | 12.59 | 14.16 | 1.57 | 15.92 | 1.93 |
26.84 | 27.88 | 1.04 | 2.38 | 0.64 | |
230.31 | 244.10 | 13.79 | 0.67 | 0.30 | |
包括 | 230.31 | 231.40 | 1.09 | 3.23 | 0.62 |
包括 | 234.95 | 236.00 | 1.05 | 1.05 | 0.38 |
LH22-56 | 11.28 | 14.75 | 3.47 | 13.90 | 1.53 |
包括 | 11.66 | 13.26 | 1.60 | 19.31 | 2.27 |
20.40 | 21.83 | 1.43 | 2.81 | 0.93 | |
包括 | 20.76 | 21.07 | 0.31 | 10.60 | 3.57 |
27.28 | 28.95 | 1.67 | 3.01 | 0.47 | |
215.50 | 224.80 | 9.30 | 4.51 | 0.72 | |
包括 | 215.50 | 216.13 | 0.63 | 1.87 | 1.18 |
包括 | 222.22 | 223.36 | 1.14 | 32.00 | 3.54 |
Core submitted for analysis was limited to visually identified mineralized intervals having at least 2% sulphide content (comprising pyrrhotite and/or arsenopyrite), generally over intervals greater than 1 metre. Several shorter intervals, having a higher proportion of sulphides (i.e. semi-massive to massive sulphides), were also sampled. Drill core was split at approximately 1 metre intervals, with one half sent to the ALS Chemex lab in Kamloops, BC for initial preparation. The remaining core was returned to the core box and stored, together with core from previous programs, in Crescent Valley, BC.
提交分析的巖芯僅限於目測確定的硫化物含量至少為2%的礦化區間(包括磁黃鐵礦和/或毒砂),礦化區間一般大於1米。還對硫化物比例較高(即半塊狀至塊狀硫化物)的幾個較短的間隔進行了採樣。鑽芯以大約1米的間隔分開,其中一半送到不列顛哥倫比亞省坎盧普斯的ALS Chemex實驗室進行初步準備。剩餘的核心被送回核心盒子,與以前項目的核心一起存儲在不列顛哥倫比亞省的新月谷。
Samples were crushed to 70% passing 2 mm and a 250 gram sub-sample then pulverized to 85% passing 75 microns. Samples were initially analyzed using the ME-MS61 package (four acid digestion followed by Inductively Coupled Plasma - Mass Spectrometry (ICP-MS) analysis). Arsenic over-limits were analyzed using the ME-OG62 package (four acid digestion followed by Inductively Coupled Plasma Atomic Emission Spectroscopy (ICP-AES)). Gold was analyzed using the AuAA23 package (Fire Assay on a 30 g separate and analyzed using Atomic Absorption). Gold over-limits were analyzed using the Au-GRA21 package (Fire Assay on a 30 g separate with a Gravimetric finish).
樣品粉碎至70%,通過2 mm和250克子樣品,然後粉碎至85%,通過75微米。樣品最初使用ME-MS61分析包(四酸消化後電感耦合等離子體質譜(ICP-MS)分析)進行分析。用ME-OG62(四酸消化-電感耦合等離子體原子發射光譜分析)分析砷超標。金的分析使用AuAA23軟件包(在30g分離器上進行火焰分析,並使用原子吸收進行分析)。使用Au-GRA21分析金的超限(30克的火試劑盒與重量法完成)。
Results are consistent with previous interpretation of multiple, structurally controlled, gold-bearing, pyrrhotite mineralized zones. These zones are interpreted to be moderately to steeply north dipping, with gold content correlated to the tenor of pyrrhotite ± arsenopyrite-bearing mineralization.
結果與以前對多個構造受控的含金磁黃鐵礦礦化帶的解釋是一致的。這些帶被解釋為中等至陡峭的北傾,金含量與磁黃鐵礦±毒砂礦化的主旨相關。
All holes intersected intervals of pyrrhotite mineralization, with only two holes LH22-51 and 54 having low-grade mineralized intervals considered too low (i.e. weakly to moderately disseminated pyrrhotite), based on visual examination, to justify sampling. The remainder of the holes contain multiple pyrrhotite mineralized intervals, with those having significant semi-massive to massive pyrrhotite mineralization submitted for quantitative analysis at this time. Intervals having low to moderate grade mineralization will be considered for analysis at a future time to provide potentially valuable information regarding the full extent of mineralized intervals in each hole. Similar weakly to moderately mineralized intervals are interpreted to have coalesced into well mineralized, high-grade gold-bearing intervals over relatively short distances between previous holes. The true thickness of the mineralized intercepts documented in the 2022 program is unknown at this time.
所有孔都與磁黃鐵礦礦化間隔相交,根據目測,只有兩個孔LH22-51和54的低品位礦化間隔被認為太低(即弱至中度浸染的磁黃鐵礦),無法證明採樣是合理的。其餘的孔洞包含多個磁黃鐵礦礦化區間,其中那些具有顯著的半塊狀至塊狀磁黃鐵礦礦化的孔洞目前提交進行定量分析。具有低至中等品位礦化的區段將被考慮在未來時間進行分析,以提供有關每個孔中礦化區段的全部範圍的潛在有價值的信息。類似的弱礦化到中等礦化區間被解釋為在以前的孔之間相對較短的距離內聚合成礦化良好的高品位含金區間。2022年計劃中記錄的礦化截獲的真實厚度目前尚不清楚。
This news release has been reviewed and approved by Rick Walker, P. Geo., who is acting as the Company's Qualified Person for the LH Property project, in accordance with regulations under NI 43-101.
根據NI 43-101的規定,本新聞稿已由擔任該公司LH地產項目合格人員的Rick Walker,P.Geo.審查和批准。
The LH Property is a gold exploration property consisting of 19 contiguous crown granted and 7 mineral claims, located approximately 7 km south of Silverton, British Columbia, on the east side of Slocan Lake. Access to the LH Property is via Highway 6 for 1.1 km south of Silverton and then via Red Mountain Road for 1.6 km. Follow to the Hewitt Mine Road for approximately 3 km to the Branch 200 Road. The Branch 200 road and, subsequently, the old mine road can be utilized by ATVs for approximately 4 km into the upper Fingland Creek drainage.
LH礦是一個金礦勘探項目,由19個相連的皇冠和7個礦藏組成,位於不列顛哥倫比亞省西爾弗頓以南約7公里處,位於斯洛坎湖東側。前往路易斯安那酒店的途徑是在西爾弗頓以南1.1公里處通過駭維金屬加工6號,然後通過紅山公路行駛1.6公里。沿休伊特礦道行駛約3公里,至200分支公路。分支200道路和隨後的舊礦場道路可供ATV使用約4公里進入Fingland Creek上游排水系統。
For further information visit the Company's website at .
欲瞭解更多信息,請訪問公司網站:。
Magnum Goldcorp Inc.
Magnum Goldcorp公司
"Douglas L. Mason"
《道格拉斯·L·梅森》
_______________________________________
_______________________________________
Douglas L. Mason, Chief Executive Officer
首席執行官道格拉斯·L·梅森
Contact:
info@waterfrontgroup.com
Tel 604.922.2030
聯繫方式:
郵箱:Info@water Frontgroup.com
電話:604.922.2030
Neither the TSX Venture Exchange nor its Regulation Services provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
多倫多證券交易所創業板交易所及其監管服務提供商(該術語在多倫多證券交易所的政策中定義)均不對本新聞稿的充分性或準確性承擔責任。
This news release includes certain statements that may be deemed "forward-looking statements" within the meaning of applicable securities legislation. All statements, other than statements of historical facts, that address such matters as future exploration, drilling, exploration activities, potential mineralization and resources and events or developments that the Company expects, are forward-looking statements and, as such, are subject to risks, uncertainties and other factors which are beyond he reasonable control of the Company. Such statements are not guarantees of future performance and actual results or developments may differ materially from those expressed in, or implied by, this forward-looking information. Any forward-looking statements are expressly qualified in their entirety by this cautionary statement. The information contained herein is stated as of the current date and subject to change after that date and the Company does not undertake any obligation to update publicly or to revise any of the forward-looking statements, whether as a result of new information, future events or otherwise, except as may be required by applicable securities laws.
本新聞稿包括可被視為適用證券法意義上的“前瞻性陳述”的某些陳述。除有關歷史事實的陳述外,涉及本公司預期的未來勘探、鑽探、勘探活動、潛在礦化和資源、事件或發展等事項的所有陳述均為前瞻性陳述,因此受本公司合理控制範圍以外的風險、不確定性和其他因素的影響。此類陳述不能保證未來的業績,實際結果或發展可能與這些前瞻性信息中所表達或暗示的大不相同。本警示性聲明明確對任何前瞻性聲明進行了完整的限定。本文中包含的信息是截至當前日期陳述的,在該日期之後可能會發生變化,公司不承擔任何公開更新或修改任何前瞻性陳述的義務,除非適用的證券法可能要求公開更新或修改任何前瞻性陳述,無論是由於新信息、未來事件還是其他原因。
This news release does not constitute an offer to sell or a solicitation of an offer to buy the securities described herein in the United States. The securities described herein have not been and will not be registered under the United States Securities Act of 1933, as amended, and may not be offered or sold in the United States or to the account or benefit of a U.S. person absent an exemption from the registration requirements of such Act.
本新聞稿不構成在美國出售或邀請購買本文所述證券的要約。本文所述證券沒有也不會根據修訂後的《1933年美國證券法》進行註冊,除非獲得該法案註冊要求的豁免,否則不得在美國境內或向美國個人的賬户或利益進行發行或出售。
NOT FOR DISSEMINATION IN THE UNITED STATES OR FOR DISTRIBUTION TO U.S. NEWSWIRE SERVICES AND DOES NOT CONSTITUTE AN OFFER OF THE SECURITIES DESCRIBED HEREIN
不得在美國傳播或分發給美國新聞通訊社服務,也不構成本文所述證券的要約
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