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Pampa Metals Intersects Wide Interval of Copper Mineralization With Bornite Rich Core in Second Drillhole at Piuquenes, San Juan Province, Argentina

Pampa Metals Intersects Wide Interval of Copper Mineralization With Bornite Rich Core in Second Drillhole at Piuquenes, San Juan Province, Argentina

Pampa Metals 在阿根廷聖胡安省皮烏克內斯的第二個鑽孔中橫穿了寬間隔的銅礦化與富含硼砂岩的岩心
Accesswire ·  03/26 19:45

VANCOUVER, BC / ACCESSWIRE / March 26, 2024 / Pampa Metals Corp. ("Pampa Metals" or the "Company") (CSE:PM)(FSE:FIRA)(OTCQB:PMMCF) is pleased to report that diamond drillhole PIU-02 (refer figure 1) was completed to a downhole depth of 870m. The hole was orientated along an east-west section, proximate to historical drillholes P4 and P2 and designed to test the lateral extension of the mineralized body, primarily along the western edge of the Piuquenes Central porphyry.

不列顛哥倫比亞省溫哥華/ACCESSWIRE/2024 年 3 月 26 日/Pampa Metals Corp.(“Pampa Metals” 或 “公司”)(CSE: PM)(FSE: FIRA)(OTCQB: PMMCF)欣然報告說,鑽石鑽孔 PIU-02 (參見圖 1) 已完工,井下深度爲 870 米。該孔沿着東西向部分定向,靠近歷史上的P4和P2鑽孔,旨在測試礦化體的橫向延伸,主要是沿着皮烏克內斯中央斑岩的西部邊緣。

Geology and Mineralization - Diamond Drillhole PIU-02

地質學和礦化-鑽石鑽孔 PIU-02

Moderate intensity porphyry A type quartz veinlets were intersected from 120 m downhole, with copper oxides evident between 218-232 m, partially coincident with a zone of moderate supergene copper enrichment from 226 to 380 m. Copper sulphide (chalcopyrite) mineralization is evident in quartz veining from 270 m.

中等強度斑岩 A 型石英脈從井下 120 米處穿過,在 218-232 m 之間有明顯的氧化銅,與 226 至 380 m 的中等超基因銅富集區部分重合。270 m 處的石英脈絡中硫化銅(黃銅礦)礦化顯而易見。

Image 1: Porphyry A type quartz stockwork veining with potassic (K-Spar) altered vein halos, supergene Cu enrichment and Cu oxides overprinting potassic altered quartz-diorite porphyry (218m)

圖片 1:Porphyry A 型石英庫存脈絡中含有鉀(K-Spar)改變的脈絡光環、超基因富集銅和銅氧化物疊印鉀改石英閃長巖斑岩(218m)

A significant increase in quartz veining is observed from 364m downhole, coincident with an increase in intermineral potassic alteration (Kfeldspar-quartz), higher magnetite content, lower presence of early biotite and the appearance of bornite and chalcopyrite mineralization. Bornite mineralization remains evident down to 610m, often more abundant than chalcopyrite, and coincident with an increased intensity of porphyry A type quartz veining and pulses of intermineral granodiorite porphyry. Bornite is disseminated in quartz veinlets, frequently intergrown with chalcopyrite. The bornite mineralized core remains open to depth.

從井下 364 米處觀察到石英脈絡顯著增加,與此同時,礦物間鉀蝕變(Kfeldspar-Quartz)的增加、磁鐵礦含量的增加、早期黑雲母的存在減少以及硼砂和黃銅礦礦化的出現。在610米以下,硼砂礦化仍然很明顯,通常比黃銅礦更豐富,並且與斑岩A型石英脈和礦物間花崗閃長巖斑岩脈衝強度的增加相吻合。硼石散佈在石英脈中,通常與黃銅礦雜交。硼砂礦化岩心仍然向深處開放。

Image 2: Intense porphyry A type quartz vein stockwork with disseminated chalcopyrite and bornite, overprinting early potassic altered diorite porphyry

圖片 2:強烈斑岩 A 型石英脈庫存,帶有浸染的黃銅礦和硼砂岩,疊印了早期的鉀蝕變閃長巖斑岩

From 610 m downhole the frequency of quartz veinlets, intermineral potassic alteration, magnetite content, and the presence of bornite decreases. Chalcopyrite-bornite mineralization remains present in the quartz veinlets, which frequently show thin Kfeldspar haloes. The outer periphery of the Piuquenes porphyry system can be observed from 690 m, with a predominance of early biotite over mafics along with disseminated magnetite, sporadic and thin quartz veinlets with a halo of potassium Kfeldspar and disseminated chalcopyrite and bornite overprinting diorite porphyry. From 690 m a late intermediate argillic event with chlorite is evident, along with veinlets and dissemination of pyrite/chalcopyrite-pyrite and specular magnetic hematite, grading to phyllic with selective chlorite-sericite and pervasive sericite veinlets, with fine dissemination of pyrite from 850 m to 870m (End of Hole).

從井下 610 米處開始,石英礦脈、礦物間鉀蝕變、磁鐵礦含量和硼礦存在的頻率會降低。石英脈中仍然存在黃銅礦-硼砂礦化作用,石英脈通常顯示出薄薄的克菲爾德斯帕光環。從690米處可以觀測到皮烏克內斯斑岩系統的外圍,早期的黑雲母占主導地位,還有浸染磁鐵礦、帶有Kfeldspar鉀光環的零星和薄石英脈以及覆蓋閃長巖斑岩的浸染黃銅礦和硼砂岩。從 690 m 開始,亞氯酸鹽的晚期中期泥質事件顯而易見,還有黃鐵礦/黃銅礦和鏡面磁性赤鐵礦的脈絡和擴散,分級爲具有選擇性亞氯酸鹽-蠶絲礦和無處不在的蠶絲礦脈的葉狀體,黃鐵礦從 850 m 到 870 m(孔的盡頭)細微擴散。

Image 3: Intense porphyry A type quartz stockwork with strong disseminated chalcopyrite mineralization, overprinting intermineral potassic altered porphyry

圖 3:強斑岩 A 型石英庫存,具有強烈的浸染性黃銅礦礦化作用,疊印礦物間鉀蝕變斑岩

Image 4: Porphyry A type quartz vein hosting coarse bornite mineralization, overprinting intermineral potassic altered porphyry

圖 4:斑岩 A 型石英脈具有粗糙的硼砂礦化作用,疊印了礦物間鉀蝕變斑岩

Assays have been prepared and dispatched to the ALS laboratory in Mendoza, results expected shortly.

化驗已經準備好並送往門多薩的ALS實驗室,預計很快就會有結果。

Joseph van den Elsen, Pampa Metals President and CEO commented: "Following on from the exceptional copper-gold intersections reported in the first hole of our maiden drill campaign at the Piuquenes Project, we are very pleased to report the presence of wide intervals of both supergene enriched and strong primary copper mineralization in the 2nd hole of our current drill program. Our maiden drill campaign continues to extend the depth and lateral extensions of mineralization at Piuquenes Central with a bornite rich core now evident and open to depth. Bornite mineralized cores are commonly associated with high grade porphyry deposits globally and we look forward to further delineating this exciting opportunity. Subsequent drill campaigns will also test the undrilled Piuquenes East porphyry target and other nearby targets identified on the property."

Pampa Metals總裁兼首席執行官約瑟夫·範登·埃爾森評論說: “繼我們在Piuquenes項目首次鑽探的第一個鑽孔中報告了特殊的銅金交叉點之後,我們很高興地報告,在2號鑽井中存在很長的超基因富集和強烈的原生銅礦化間隔 我們當前鑽探計劃的漏洞。我們的首次鑽探活動繼續擴大Piuquenes Central礦化的深度和橫向延伸,富含硼砂岩的岩心現已顯而易見,並向深度開放。Bornite礦化岩心通常與全球高品位斑岩礦牀有關,我們期待進一步描繪這一令人興奮的機會。隨後的鑽探活動還將測試未鑽探的Piuquenes East斑岩目標以及該物業上確定的其他附近目標。”

Figure 1: PIU-02 Schematic Cross Section

圖 1:PIU-02 示意圖橫截面

ON BEHALF OF THE BOARD INVESTOR CONTACT

代表董事會投資者聯繫人

Joseph van den Elsen | President & CEO Joseph van den Elsen | Joseph@pampametals.com

約瑟夫·範登埃爾森 | 總裁兼首席執行官約瑟夫·範登埃爾森 | Joseph@pampametals.com

ABOUT PAMPA METALS

關於 PAMPA 金屬

Pampa Metals is a copper-gold exploration company listed on the Canadian Stock Exchange (CSE:PM), Frankfurt (FSE:FIRA), and OTC (OTCQB:PMMCF) exchanges.

Pampa Metals是一家銅金勘探公司,在加拿大證券交易所(CSE: PM)、法蘭克福(FSE: FIRA)和場外交易所(場外交易代碼:PMMCF)上市。

In November 2023, the Company announced it had entered into an Option and Joint Venture Agreement for the acquisition of an 80% interest in the Piuquenes Copper-Gold Porphyry Project in San Juan Province, Argentina. Reported intervals of significant copper and gold mineralization at Piuquenes Central include:

2023年11月,該公司宣佈已簽訂期權和合資協議,以收購阿根廷聖胡安省皮烏肯斯銅金斑岩項目80%的權益。Piuquenes Central 報告的顯著銅金礦化間隔包括:

413.5 m@ 0.47% Cu, 0.52 g/t Au (0.87% CuEq)* (167-580.5 m);

413.5 m@ 0.47% 銅,0.52 g/t 金 (0.87% cueQ) * (167-580.5 m);

422 m @ 0.48% Cu, 0.61 g/t Au, 2.9 g/t Ag (1.00% CuEq)* (198 - 620m);

422 m @ 0.48% 銅,0.61 g/t 金,2.9 g/t Ag (1.00% cueQ) * (198-620 米);

including 132m @ 0.71% Cu, 0.85 g/t Au, 4.3 g/t Ag (1.45% CuEq)* (220 - 352m);

包括 132m @ 0.71% 銅、0.85 g/t Au、4.3 g/t Ag (1.45% CueQ) * (220-352m);

including 80m @ 0.6% Cu, 0.77 g/t Au, 3.2 g/t Ag (1.30% CuEq)* (468 - 548m)

包括 80m @ 0.6% Cu、0.77 g/t Au、3.2 g/t Ag (1.30% CueQ) * (468-548 m)

558.2 m @ 0.38% Cu, 0.42 g/t Au, 2.4 g/t Ag (0.73% CuEq)* (362-920.2 m EOH)

558.2 m @ 0.38% 銅,0.42 g/t 金,2.4 g/t Ag (0.73% cueQ) * (362-920.2 m EOH)

including 130 m @ 0.81% Cu, 0.6 g/t Au, 4 g/t Ag (1.31 % CuEq)* (362-492 m)

包括 130 m @ 0.81% 銅、0.6 g/t Au、4 g/t Ag (1.31% CueQ) * (362-492 m)

Qualified Person

合格人員

Technical information in this news release has been approved by Mario Orrego G. Mr. Orrego G. is a Geologist, a Registered Member of the Chilean Mining Commission and a Qualified Person as defined by National Instrument 43-101. Mr. Orrego G. is a consultant to the Company.

本新聞稿中的技術信息已獲得Mario Orrego G. 的批准。Orrego G. 先生是一名地質學家、智利礦業委員會的註冊成員和國家儀器43-101定義的合格人士。Orrego G. 先生是該公司的顧問。

* %CuEq values are calculated based on copper and gold metal prices: Cu = US$3.20/lb, Au = US$1,700/oz and Ag = US$ 20/oz. The formula utilized to calculate %CuEq is: Cu Eq Grade (%) = Cu Head Grade (%) + [(Au Head Grade (g/t) / 31.104) * (Au Price (US$/oz) / Cu Price (US$/lb) / 22.04) + [(Ag Head Grade (g/t) / 31.104) * (Ag Price (US$/oz) / Cu Price (US$/lb) / 22.04.

* %cueQ 值根據銅和金金屬價格計算:銅 = 3.20 美元/磅,金 = 1,700 美元/盎司,銀 = 20 美元/盎司。用於計算 %cueQ 的公式是:銅當量等級 (%) = 銅頭等級 (%) + [(金頭等級 (g/t) /31.104) * (澳元/盎司) /銅價格 (美元/磅)/22.04) + [(銀頭等級(g/t)/31.104)*(銀價(美元/盎司)/銅價(美元/磅)/22.04。

Neither the CSE nor the Investment Industry Regulatory Organization of Canada accepts responsibility for the adequacy or accuracy of this release.

CSE和加拿大投資行業監管組織均不對本新聞稿的充分性或準確性承擔責任。

FORWARD-LOOKING STATEMENT

前瞻性陳述

This news release contains certain statements that may be deemed "forward-looking statements". All statements in this release, other than statements of historical fact, that address events or developments that Pampa Metals expects to occur, are forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words "expects" and similar expressions, or that events or conditions "will" or "may" occur. These statements are subject to various risks. Although Pampa Metals believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guaranteeing of future performance and actual results may differ materially from those in forward-looking statements.

本新聞稿包含某些可能被視爲 “前瞻性陳述” 的陳述。除歷史事實陳述外,本新聞稿中涉及Pampa Metals預計將發生的事件或事態發展的所有陳述均爲前瞻性陳述。前瞻性陳述不是歷史事實,通常以 “期望” 一詞和類似表達方式來識別,或者事件或條件 “將” 或 “可能” 發生,但並非總是如此。這些聲明存在各種風險。儘管Pampa Metals認爲此類前瞻性陳述中表達的預期是基於合理的假設,但此類陳述並不能保證未來的業績,實際業績可能與前瞻性陳述中的業績存在重大差異。

SOURCE: Pampa Metals Corp.

來源:潘帕金屬公司


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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