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Aurwest Announces Phase 2 Drill Results Including 5.43g/t Au In DDH PL-22-12 at Paradise Lake Gold Project Newfoundland

Aurwest Announces Phase 2 Drill Results Including 5.43g/t Au In DDH PL-22-12 at Paradise Lake Gold Project Newfoundland

Aurwest宣佈第二階段鑽探結果,包括紐芬蘭天堂湖黃金項目的5.43克/噸DDH PL-22-12中的Au
newsfile ·  2022/09/22 02:00

Calgary, Alberta--(Newsfile Corp. - September 21, 2022) - Aurwest Resources Corporation (CSE: AWR) ("Aurwest" or the "Company") announces final drilling results from its Phase 2 drilling program completed at its Paradise Lake gold project in Central Newfoundland. Phase 2 consisted of seven holes totaling 1,050-meters, to follow-up intervals of low-grade gold mineralization intersected by Phase 1 drilling. The drilling program at Paradise Lake consisted of 18 drill holes totaling 3,796m.

加拿大阿爾伯塔省卡爾加里-(Newsfile Corp.-2022年9月21日)-Aurwest Resources Corporation(CSE:AWR) ("奧韋斯特“或”公司“)宣佈在其位於紐芬蘭中部的天堂湖金礦項目完成的第二階段鑽探計劃的最終鑽探結果。第二階段包括七個總計1,050米的孔,以跟進與第一階段鑽探相交的低品位金礦化。天堂湖的鑽探計劃包括18個鑽孔,總計3796米。

Highlights of the drilling program are:

鑽探計劃的亮點是:

  • Hole DDH PL-22-12 intersected 5.43 g/t Au over a 0.5m core interval in PL-22-12.
  • Four of the seven drill holes completed as part of the Phase 2 drilling intersected 16 intervals with greater than 0.1g/t gold over core intervals ranging from 0.5 to 10.90m.
  • The 18 hole (3,796m) program returned 50 intervals with gold concentration in excess of 0.1g/t over core intervals ranging from 0.5 to 10.9 m widths.
  • Higher grade intervals of include; 6.21g/t Au over 0.5m in DDH PL-22-01, 6.00g/t Au over 0.5m and 7.75g/t Au over 0.5m core intervals in DDH PL-22-07and 5.43g/t Au over a 0.5m core interval in DDH PL-22-12.
  • Native gold was observed in quartz veins in DDH PL-22-07.
  • Holes PL-22-01 and PL-22-16 are interpreted to have intersected the same mineralized zone estimated to be over a strike length of 250 meters beneath Twin Ponds. This zone is open to the East and West.
  • DDH PL-22-12井在PL-22-12井的0.5m巖心間隔內相交5.43g/t Au。
  • 作為第二階段鑽探的一部分,完成的七個鑽孔中有四個相交於16個井段,巖心井段從0.5米到10.90米,含金量超過0.1g/t。
  • 18孔(3796米)程序返回了50個巖層,巖心寬度從0.5米到10.9米不等,黃金濃度超過0.1g/t。
  • 較高品位段包括:DDH PL-22-01的0.5m以上Au 6.21g/t,DDH PL-22-07 0.5m巖心段Au 6.00g/t,0.5m巖心段Au 7.75g/t,DDH PL-22-12 0.5m巖心段Au 5.43g/t。
  • 在DDH PL-22-07的石英脈中觀察到自然金。
  • 據解釋,孔PL-22-01和PL-22-16與同一礦化帶相交,據估計,該礦化帶在雙池塘下的走向長度超過250米。這一區域向東西兩面開放。

Mr. Colin Christensen stated, "The drilling intersected multiple widths of gold mineralization ranging from near surface to depth of approximately 180m below surface localized along the contacts of the Twin ponds syenite intrusions. The multiple episodes of gold bearing quartz veins suggest a once active hydrothermal center carrying native gold, arsenopyrite and pyrite mineralization. It is believed that secondary faults/structures intersecting the main Northeast tending intrusive corridor may also contain significant gold mineralization as is supported by drilling results and the recent discovery of gold mineralization in outcrop 4.5km northwest of Paradise Lake."

Colin Christensen先生説:“鑽探涉及多個寬度的金礦化,從近地表到地表以下約180米的深度,沿着雙子池正長巖侵入體的接觸定位。多期含金石英脈表明,一個曾經活躍的熱液中心攜帶着自然金、毒砂和黃鐵礦礦化。鑽探結果和最近在天堂湖西北4.5公里露頭髮現的金礦牀支持,與東北主要傾向侵入走廊相交的次級斷層/構造也可能包含重要的金礦化。”

Phase 2 Drilling:

第二階段鑽探:

The target tested by the drilling program is part of a nearly 10 km long trend identified from surface samples that returned gold concentration ranging from 0.05 to 144.7g/t gold. Numerous chargeability targets remain to be tested, identified from the 2021 IP geophysical survey.

鑽探計劃測試的目標是近10公里長趨勢的一部分,該趨勢是從地表樣品中發現的,返回的黃金濃度從0.05克/噸到144.7克/噸不等。從2021年IP地球物理調查中確定的許多可收費目標仍有待測試。

Hole PL-22-16 intersected a 10.9-meter core interval of 0.21 g/t Au. This zone of shallow pyrite-arsenopyrite mineralization is apparent in the 2021 IP geophysical results as a chargeability high. The host rock consists of various phases of syenite, diorite and mafic dykes with local xenoliths of other intrusive and felsic volcanic rocks. Alteration consists of variable degrees of fine-grained interstitial chlorite-carbonate-K-feldspar-pyrite and quartz-sericite-ankerite. Quartz veins vary from laminated, massive, breccia and stockwork-like. They are often vuggy and contain fine-grained pyrite and arsenopyrite. Only veins that contain significant arsenopyrite-pyrite content returned significant gold concentrations. Mineralized intervals containing greater than 0.1g/t gold from Phase 2 program are set out in Table-1 below:

PL-22-16孔與10.9米長的巖心相交,巖心厚度為0.21g/t Au。這一淺層黃鐵礦-毒砂成礦帶在2021年IP地球物理結果中表現為高充電性。主巖由不同階段的正長巖、閃長巖和鎂鐵質巖牆組成,局部包體為其他侵入巖和長英質火山巖。蝕變由不同程度的綠泥石-碳酸鹽-鉀長石-黃鐵礦和石英-絹雲母-鐵角閃石組成。石英脈有層狀、塊狀、角礫巖和網狀等。它們通常是洞穴狀的,含有細粒黃鐵礦和毒砂。只有含有大量毒砂-黃鐵礦含量的礦脈才能返回大量的金。第二階段項目中含金量大於0.1g/t的礦化間隔如下表1所示:

Notes: The cut-off selected for determining the weighted average for the mineralized intervals was 0.1g/t gold. No limitation placed on the sample interval. Gold grades are rounded. Intervals reported in table are core intervals and do not represent true width.

備註確定成礦層段加權平均值的下限為0.1g/t金。對採樣間隔沒有限制。黃金等級是四捨五入的。表中報告的間隔是核心間隔,並不代表真實寬度。

PL-22-12 (161m, 291 o, -45 o) is located 50m south of collar PL-22-01/02. It targeted a 400m wide chargeability high beneath the lake and corresponding gold grades and pyrite-arsenopyrite intersected in hole PL-22-01/02. The hole collared into cross bedded siltstone from 22-25.3m depth. Syenite was then intersected until end of hole with at least 3 distinct chilled margins. Eleven zones from 1-10m wide contain trace amounts, up to 5% fine-grained pyrite-arsenopyrite, disseminated, fracture filling and in veins up to 6cm wide. Alteration in the syenite includes variable K-feldspar-chlorite-leucoxene-ankerite and veins of quartz-chlorite-ankerite/calcite.

PL-22-12(161m, 291 o, -45 o)位於領口以南50米處,PL-22-01/02。它的目標是湖下400米寬的可充電性,以及在PL-22-01/02孔中相交的相應的黃金品位和黃鐵礦-毒砂。該井深22-25.3米,鑽穿交錯層狀粉砂巖。然後正長巖被相交,直到孔的末端,至少有3個明顯的冷卻邊緣。11個1-10米寬的區域含有微量,高達5%的細粒黃鐵礦-毒砂,呈浸染狀、裂縫充填和脈體寬達6釐米。正長巖中的蝕變有多變的鉀長石-綠泥石-白雲母-鐵角閃石和石英-綠泥石-鐵白雲母/方解石脈。

PL-22-13 (164.2m, 070 o, -45 o) is located on the northwest side of Twin Pond targeting an area of angular quartz veins with up to 144 g/t Au. The hole collared into syenite at 22.2m and continued until the end of the hole. Interbedded bedded greywacke/siltstone was intersected over the core interval from 73 to150m. An intermediate dyke occurs from 69-73m. Only trace amounts of pyrite occur in moderately altered syenite and siltstone. Fine-grained pyrite occurs as disseminations, fracture fill, and in breccias/ fault zones up to 1.5m wide. Alteration includes moderate, interstitial to pervasive pink K-feldspar, chlorite-leucoxene-calcite-ankerite.

PL-22-13(164.2m, 070 o, -45 o)位於Twin Pond的西北側,目標是一片角狀石英脈區域,Au含量高達144克/噸。該洞在22.2米處進入正長巖,並一直持續到洞的盡頭。在73~150m的巖心段,夾層雜砂巖/粉砂巖相交。中級堤防出現在69-73m處。中等蝕變正長巖和粉砂巖中只有微量的黃鐵礦。細粒黃鐵礦以滲漏、裂隙充填的形式賦存於寬達1.5米的角礫巖/斷裂帶中。蝕變類型為中等、間隙至瀰漫的粉紅色鉀長石、綠泥石-白蠟石-方解石-鐵角閃石。

PL-22-14 (159m, 040 o, -45 o) is located 160m west of PL-22-13. It targeted a broad positive resistivity signature. The hole collared into sediments consisting of cross bedded greywacke and maroon siltstone until end of hole. Bedding appears steeply dipping to the east. The syenite contact was not intersected as was anticipated. Two mafic dykes were intersected at 20 and 70m depth and are 1 and 3.5m wide. Only trace amounts of fine-grained pyrite and chalcopyrite were intersected in the mafic dykes.

PL-22-14(159m, 040 o, -45 o)位於PL-22-13以西160米處。它的目標是一個廣泛的正電阻率特徵。井眼由交錯層理的雜砂巖和栗色粉砂巖組成,直至井底。層理似乎向東陡峭傾斜。正長巖的接觸並沒有像預期的那樣相交。兩條鎂鐵質巖牆相交,深度分別為20米和70米,寬分別為1米和3.5米。鎂鐵質巖脈中只有少量細粒黃鐵礦和黃銅礦相交。

PL-22-15 (155m, 105 o, -45 o) is located 290m west of collar PL-22-01/02. It targeted the mineralization intersected in hole PL-22-01/02, and chargeability high beneath North Twin Pond. It collared into siltstone from 12-17m depth. Syenite was intersected from 17-34m, 35-41m, and 43-155m depth, each separated by thin bedded siltstone and greywacke. The intrusions range from glassy pink to grey plag-phyric and medium grained holocrystalline. Numerous zones contain trace amounts of fine-grained, disseminated pyrite and in quartz veins 1-5cm thick. Alteration includes patchy, pink K-feldspar-chlorite-leucoxene-ankerite alteration.

PL-22-15(155m, 105 o, -45 o)位於環PL-22-01/02以西290米處。它的目標是與PL-22-01/02孔相交的礦化,以及北雙子池下方的高可充電性。它從12-17米深進入粉砂巖。正長巖相交深度分別為17~34m、35~41m、43~155m,分別由薄層粉砂巖和雜砂巖隔開。侵入巖範圍從玻璃色粉紅色到灰色原狀和中粒全晶。許多帶中含有微量的細粒浸染狀黃鐵礦,在1-5釐米厚的石英脈中。蝕變包括斑片狀、粉紅色鉀長石-綠泥石-白蠟石-鐵角閃石蝕變。

PL-22-16: (137m, 115o/-45 o) is located on the west side of North Twin Pond drilling southeast towards hole PL-22-12 and 100m south of PL-22-15 along the same linear syenite intrusion. The hole collared into interbedded green-grey wacke and maroon argillite from 8.7-58m depth and syenite intrusion to end of hole. Pyrite-arsenopyrite ranges from trace amounts up to 7% interval within the syenites over broad intervals up to 15m. Fault zones and brecciated syenite contain arsenopyrite mineralization related to quartz veining. Alteration includes pervasive k-feldspar with zones of strong ankerite, sericite and chlorite.

PL-22-16:(137m, 115o/-45 o)位於北雙池鑽井的西側,朝孔PL-22-12和PL-22-15以南100米,沿同一線性正長巖侵入。該井眼由8.7~58m深的綠灰色泥巖和褐泥巖互層組成,正長巖侵入至井底。黃鐵礦-毒砂的範圍從正長巖中微量到7%的間隔,範圍很寬,最長可達15m。斷裂帶和角礫狀正長巖中含有與石英脈有關的毒砂礦化。蝕變包括廣泛分佈的鉀長石,並有較強的鐵角閃石、絹雲母和綠泥石。

PL-22-17: (122m, 295o/-45 o) is located roughly 50m south of hole PL-22-07 testing the same mineralized structure observed in PL-22-07. The hole collared in syenite and intersected 3 distinct syenites before contacting interbedded green-grey wacke and maroon argillite. Five weakly mineralized zones are identified. Based on analytical results, no intervals contained greater that 100 pb gold. Quartz veins are very thin and contain trace amounts of pyrite. Alteration is patchy and consists of k-spar, sericite, chlorite and ankerite, where ankerite and sericite is local, and chlorite and k-spar are more prominent.

PL-22-17:(122m, 295o/-45 o)位於孔PL-22-07以南約50米處,測試與在PL-22-07中觀察到的相同礦化結構。該孔被正長巖套住,與3個截然不同的正長巖相交,然後與互層的綠灰泥巖和褐泥巖接觸。共識別出5個弱礦化帶。根據分析結果,沒有任何一段時間的黃金含量超過100 PB。石英脈非常薄,含有微量的黃鐵礦。蝕變呈斑塊狀,由鉀石、絹雲母、綠泥石和鐵閃石組成,其中鐵閃石和絹雲母為局部蝕變,綠泥石和鉀石較為突出。

PL-22-18: (116m, 025o/-45 o) is located at the same pad as hole PL-22-07 drilling northeast. The hole collared into syenite at 9.8m depth. Mineralization is hosted mainly within a darker diorite altered by quartz-calcite-ankerite-pyrite-arsenopyrite related to strong fracturing. It also contains pervasive K-feldspar and sericite with local ankerite. It contains 1-3% pyrite-arsenopyrite mineralization over several zones up to 3m wide. The diorite has a faulted lower contact hosting local arsenopyrite mineralization.

PL-22-18:(116m, 025o/-45 o)位於與向東北鑽井的PL-22-07井相同的墊層上。這個洞在9.8米深的地方鑽進了正長巖。礦化主要賦存於與強烈破裂有關的深色閃長巖中,受石英-方解石-鐵角閃石-黃鐵礦-毒砂的蝕變作用影響。它還含有普遍存在的鉀長石和絹雲母以及當地的鐵白雲母。它包含1-3%的黃鐵礦-毒砂礦化,分佈在幾個寬達3米的區域。閃長巖具斷裂下接觸帶,賦存局部毒砂礦化。

Exploration Update:

探索更新:

Property wide prospecting and mapping at the Miguel's Lake, Stony Caldera, and Paradise Lake Projects began in May. In total 530 rock samples have been collected from outcrop, subcrop and angular float. Results have been received for 306 of these samples, 29 of which returned >50 ppb Au up to 4.03 g/t Au. Prospecting has identified several areas of outcropping quartz veining and pyrite-mineralization with rare visible gold. This area is 4.5 km northwest of Phase 1 and Phase 2 drilling area at Twin Ponds. Detailed spot chip sampling of the outcrop returned from 1.60 to 4.03 g/t gold, and 3.06 g/t silver in four samples over an exposure of ~15 meters length. Channel sampling is planned to further assess the potential widths and grade of this high priority target.

Miguel‘s Lake、Stony Caldera和Paradise Lake項目的全物業勘探和測繪於5月開始。共採集露頭、次露頭和角狀漂浮巖樣530個。已收到306個樣品的結果,其中29個樣品的金回收率>50 ppb,最高可達4.03克/噸。勘探發現了幾個露頭的石英脈和黃鐵礦礦化區域,具有稀有的可見金。該區域位於第一階段鑽探區域西北4.5公里處,第二階段鑽探區域位於雙池塘。露頭的詳細斑點芯片樣本在約15米長的曝光時間內返回了1.60到4.03克/噸的金,以及3.06克/噸的銀。計劃進行渠道抽樣,以進一步評估這一高優先級目標的潛在寬度和等級。

Exploration Model:

探索模式:

The Paradise Lake-Stony Caldera properties are considered to have potential to host "Orogenic" and "Intrusive Related" styles of gold mineralization comparable to the Valentine Lake, Cape Ray, Moosehead, and Queensway gold deposits. They are hosted within the Cape-Ray-Valentine Lake ("CRVL") structural zone. Linear magnetic intrusions of granodiorite/syenite occur in the vicinity of Twin Ponds-Paradise Lake. They are situated along primary or secondary structures to the CRVL. Airborne magnetic data and ground IP surveys have revealed coincident anomalies and multiple phases of intrusive activity. High-grade gold bearing, "leakage" structures have been sampled at surface and intersected in drilling. Similar structural zones elsewhere in the property have been targeted for follow up exploration in 2022.

Paradise Lake-Stony Caldera礦藏被認為具有與瓦倫丁湖、雷角、慕斯黑德和金鐘道金礦牀相媲美的“造山型”和“侵入型”金礦化類型的潛力。它們位於開普雷瓦倫丁湖(“CRVL”)構造帶內。花崗閃長巖/正長巖的線性磁性侵入作用發生在雙池-天堂湖附近。它們位於CRVL的初級或次級結構上。航磁數據和地面激電探測揭示了一致的異常和多階段的侵入活動。高品位含金“滲漏”構造已在地面取樣,並在鑽探中交會。該地產其他地方類似的構造帶已被確定為2022年的後續勘探目標。

Analytical Procedures:

分析方法:

Sample preparation and analytical work for drill core was completed by Bureau Veritas Commodities Canada Inc. ("BV") located in Vancouver B.C. BV has an ISO/IEC 17025 certification. Sample preparation followed BV's code PRP70-1kg. Gold and 36 trace elements concentrations is determined using BV's code AQ202, ICP-ES/MS on a 30g sample. Aurwest's QA/QC protocol includes geotechnical measurements, photographs, detailed geological logging and insertion of Standard Reference Material and blanks in the sample streams. A selection of 93 sample pulps with >50ppb Au were run by fire assay and comparatively analyzed. The results when compared to ICP ES/MS were mostly within a standard deviation of variance. Rock sampled collected from 2022 are being send to Eastern Analytical in Springdale, Newfoundland for gold by fire assay and 34 trace elements by ICP-ES/MS.

鑽芯的樣品準備和分析工作由位於不列顛哥倫比亞省温哥華的加拿大VERITAS商品局(“BV”)完成。BV擁有國際標準化組織/國際電工委員會17025認證。樣品製備遵循BV的編碼PRP70-1 KG。金和36種痕量元素濃度的測定使用BV的代碼AQ202,電感耦合等離子體發射光譜儀/質譜儀對30g樣品進行測定。AurWest的質量保證/質量控制協議包括巖土測量、照片、詳細的地質記錄以及在樣品流中插入標準參考材料和空白。對93個Au>50 ppb的紙漿進行了火法測定和對比分析。與電感耦合等離子體發射光譜儀/質譜儀比較,結果大多在標準偏差範圍內。從2022年採集的巖石樣品正被送往紐芬蘭斯普林代爾的東方分析公司,用火法化驗黃金,用電感耦合等離子體質譜/質譜儀測定34種微量元素。

Qualified Person:

合格人員:

Elmer B. Stewart, MSc. P. Geol., is the Company's independent, nominated Qualified Person pursuant to National Instrument 43-101, Standards for Disclosure for Mineral Projects, and has reviewed and approves the scientific and technical information disclosed in this news release.

埃爾默·B·斯圖爾特,理學碩士根據國家儀器43-101《礦產項目披露標準》,P.Geol.是公司的獨立指定合格人士,並已審查和批准本新聞稿中披露的科學和技術信息。

On Behalf Of Aurwest resources Corporation

我代表Aurwest資源公司

"Colin Christensen"
President and Chief Executive Officer

《科林·克里斯滕森》
總裁與首席執行官

For additional information please contact:
Colin Christensen
Telephone: (403) 483-8363
Email: cchristensen@aurwestresources.com
Website: aurwestresources.com

如需更多信息,請聯繫:
科林·克里斯滕森
電話:(403)483-8363
電子郵件:cchristensen@aurwestresource ces.com
網址:aurwestresource ces.com

About Aurwest Resources Corporation

關於Aurwest資源公司

Aurwest is a Canadian-based junior resource company focused on the acquisition, exploration, and development of gold properties in Canada. The Company currently has three Option Agreements to earn a 100% interest in Paradise Lake and Stony Caldera projects covering a 57,600-hectare (576 sq kms) package of gold exploration licenses within the emerging Central Newfoundland gold district. The Company also currently holds a 100% interest in the 28,294-hectare Stellar/Stars porphyry copper project, located approximately 25 kilometers southwest of Houston, British Columbia.

Aurwest是一家總部位於加拿大的初級資源公司,專注於收購、勘探和開發加拿大的黃金資產。本公司目前擁有三份期權協議,以賺取Paradise Lake和Stony Caldera項目的100%權益,該項目涵蓋新興的中紐芬蘭金礦區內57,600公頃(576平方公里)的一攬子黃金勘探許可證。本公司目前還持有位於不列顛哥倫比亞省休斯敦西南約25公里的28,294公頃的Stella/Stars斑巖銅礦項目的100%權益。

Forward-Looking Information

前瞻性信息

Statements included in this announcement, including statements concerning our plans, intentions, and expectations, which are not historical in nature are intended to be, and are hereby identified as "forward-looking statements." Forward-looking statements may be identified by words including "anticipates," "believes", "intends", "estimates", "expects" and similar expressions. The Company cautions readers that forward-looking statements, including without limitation those relating to the Company's future operations and business prospects, are subject to certain risks and uncertainties that could cause actual results to differ materially from those indicated in the forward-looking statements. Readers are advised to rely on their own evaluation of such risks and uncertainties and should not place undue reliance on forward-looking statements. Any forward-looking statements are made as of the date of this news release, and the Company assumes no obligation to update the forward-looking statements, except in accordance with the applicable laws.

本公告中包含的聲明,包括與我們的計劃、意圖和預期有關的聲明,都是非歷史性的聲明,特此確認為“前瞻性聲明”。前瞻性陳述可以通過包括“預期”、“相信”、“打算”、“估計”、“預期”和類似表述的詞語來識別。公司提醒讀者,前瞻性陳述,包括但不限於與公司未來運營和業務前景有關的陳述,會受到某些風險和不確定因素的影響,這些風險和不確定因素可能會導致實際結果與前瞻性陳述中所述的大不相同。建議讀者依靠自己對此類風險和不確定性的評估,不應過度依賴前瞻性陳述。任何前瞻性陳述都是在本新聞稿發佈之日作出的,公司不承擔更新前瞻性陳述的義務,除非依照適用的法律。

The Canadian Securities Exchange has not reviewed and does not accept responsibility for the adequacy or accuracy of this release.

加拿大證券交易所沒有對本新聞稿的充分性或準確性進行審查,也不承擔任何責任。

To view the source version of this press release, please visit

要查看本新聞稿的源版本,請訪問

譯文內容由第三人軟體翻譯。


以上內容僅用作資訊或教育之目的,不構成與富途相關的任何投資建議。富途竭力但無法保證上述全部內容的真實性、準確性和原創性。
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