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Antler Gold Commences Gold Exploration Program at Paresis Gold Project in Namibia

Antler Gold Commences Gold Exploration Program at Paresis Gold Project in Namibia

Antler Gold 在納米比亞的 Paresis 黃金項目啓動黃金勘探計劃
newsfile ·  02/05 23:48

Halifax, Nova Scotia--(Newsfile Corp. - February 5, 2024) - Antler Gold Inc. (TSXV: ANTL) ("Antler" or "Company") is pleased to announce the commencement of exploration work at the Paresis Gold Project in north central Namibia.

新斯科舍省哈利法克斯--(Newsfile Corp.,2024年2月5日)——Antler Gold Inc.(多倫多證券交易所股票代碼:ANTL)(“Antler” 或 “公司”)欣然宣佈,納米比亞中北部的帕雷西斯金礦項目開始勘探工作。

Highlights

亮點

  • The Paresis Project area covers approximately 21,000 ha within the highly prospective "gold corridor" of Namibia that hosts the Otjikoto Gold Mine (B2Gold) and the Ondundu and Eureka Gold Projects (Osino Resources).
  • A conceptual project in an area with a complex deformation and magmatic history provides structural complexity and lithological variations, presenting potential for both intrusion-related and orogenic-style gold deposits.
  • Prioritized Target Areas: Review of historical data (geochemical and airborne geophysical surveys), regional government data, and satellite imagery has allowed for the identification and prioritization of lithological and structural target areas.
  • 帕雷西斯項目區域佔地約21,000公頃,位於納米比亞極具前景的 “黃金走廊” 內,該走廊是奧奇科託金礦(B2Gold)以及昂敦杜和尤里卡黃金項目(奧西諾資源)的所在地。
  • 在一個具有複雜變形和岩漿歷史的地區進行的概念性項目提供了結構複雜性和巖性變化,這爲與入侵相關的和造山風格的金礦牀提供了潛力。
  • 優先目標區域:審查歷史數據(地球化學和航空地球物理調查)、地區政府數據和衛星圖像,可以確定巖性和結構目標區域並對其進行優先排序。

"I am excited to share an update on our exploration efforts at the Paresis Gold Project, a key initiative in Namibia's renowned 'gold corridor'. In line with Antler's core strategy, the Company intends on finding a suitable partner to progress the project through an earn-in or similar agreement, aimed at maximizing future discovery benefits for our shareholders. I am grateful for our team's dedication and I look forward to sharing additional progress in the near future," said Christopher Drysdale, CEO of Antler Gold Inc.

“我很高興分享我們在Paresis黃金項目勘探工作的最新情況,這是納米比亞著名的'黃金走廊'的一項重要舉措。根據Antler的核心戰略,公司打算通過盈利協議或類似協議尋找合適的合作伙伴來推進該項目,旨在最大限度地提高股東未來的發現收益。我感謝我們團隊的奉獻精神,我期待在不久的將來分享更多進展。” Antler Gold Inc.首席執行官克里斯托弗·德賴斯代爾說。

Exploration Strategy

探索策略

The exploration program will roll out in phases, starting with geological mapping and grab rock chip sampling as phase one, followed by a geochemical sampling program in the second phase, depending on initial rock chip assay results. Prospective lithological units of the Okonguarri and Karibib Formations (both Swakop Group) underlie the license area, however, the majority of the area is covered by soil and calcrete.

勘探計劃將分階段推出,第一階段是地質測繪和岩屑採樣,然後是第二階段的地球化學採樣計劃,視初始岩屑分析結果而定。Okonguarri和Karibib地層(均爲Swakop集團)的潛在巖性單位位於許可區的下方,但是,該區域的大部分被土壤和鈣質混凝土覆蓋。

The Okonguarri Formation is the hosting stratigraphic unit at the Otjikoto Gold Mine (B2Gold) and at the Eureka Gold Project (Osino Resources), while the Karibib Formation is host to gold mineralization at various gold occurrences (Onguati, Goldkuppe, Erindi) in the Central Zone of the Damara Belt, including the Navachab Gold Mine (QKR) (along with the Arandis Formation) (Figures 1, 2 and 3).

奧孔瓜裏組是奧奇科託金礦(B2Gold)和尤里卡金礦項目(奧西諾資源)的託管地層單元,而卡里比布組是達馬拉地帶中央區域各種金礦點(昂瓜蒂、戈德庫佩、埃林迪)的金礦化場所,包括納瓦查布金礦(QKR)(以及阿蘭迪斯形成)(圖 1、2 和 3)。

The Paresis Gold Project

帕雷西斯黃金項目

The Paresis Gold Project is currently made up of Exclusive Prospecting License ("EPL") 8711 of approx. 21,000 hectares and another EPL application situated between the towns of Otjiwarongo and Outjo, ~290 km from the capital Windhoek, in north central Namibia, within the Northern Zone (NZ) of the Damara Orogenic Belt. The NZ is host to numerous mineral deposits, including the Otjikoto Gold Mine (B2Gold), the Ondundu and Eureka Gold Projects (Osino Resources), the Okanjande Graphite deposit (Northern Graphite) and the Okorusu Fluospar Mine to name a few, evidencing this geological environment's fertile nature (Figures 1 and 2).

帕雷西斯黃金項目目前由佔地約21,000公頃的8711份獨家勘探許可證(“EPL”)和另一份位於奧吉瓦龍戈鎮和奧喬鎮之間的EPL申請組成,距離納米比亞中北部首都溫得和克約290公里,位於達馬拉造山帶北部區域(新西蘭)內。新西蘭擁有衆多礦牀,包括奧奇科託金礦(B2Gold)、昂敦杜和尤里卡黃金項目(奧西諾資源)、奧坎揚德石墨礦牀(北方石墨)和奧科魯蘇氟石礦等,證明了這種地質環境的肥沃性質(圖1和2)。

Outcrop on the license area is moderately to well-exposed, comprising rocks from the pre-Damara Basement, Nosib Group and Swakop Group (lower Damara Supergroup) (Figure 3, Table 1). The pre-Damara Basement has been tightly folded into km-scale upright folds striking roughly east-west. The Damara sequence has been intruded by younger Karoo-aged dolerite dykes and the Jurassic to Cretaceous-aged Paresis Igneous Complex (PIC).

許可區域的露頭暴露在中度至較高水平,包括來自前達馬拉地下室、諾西布組和斯瓦科普組(下達馬拉超級群)的岩石(圖3,表1)。達馬拉之前的地下室已緊緊地摺疊成千米級的直立褶皺,大致向東西方向。達馬拉序列受到了年輕的卡羅時代的白雲岩堤壩和侏羅紀至白堊紀時代的帕雷西斯火成複合體(PIC)的干擾。

Table 1: NZ stratigraphy of the Paresis tenement.

表 1: 帕雷西斯物業單位的新西蘭地層學.

Sequence Group Subgroup Formation Lithology
Paresis Igneous Complex (PIC) bimodal volcanics/extrusives, acidic and alkaline intrusives
Karoo Supergroup dolerite dykes
Damara Supergroup Swakop Navachab Karibib marble
limestone, schist, quartzite
Usakos Okonguarri (Arandis equivalent) schist, greywacke, limestone
Chuos diamictite, iron-formation
Nosib
Etusis or equivalent arkosic quartzite, meta-arkose, conglomerate, limestone, shale, gneiss
Pre-Damara Basement - Huab Metamorphic Complex gneiss, minor amphibolite
順序 小組 子組 形成 巖性學
麻疹火成複合物 (PIC) 雙峯火山岩/擠出物、酸性和鹼性侵入物
Karoo 超級群組 白雲岩堤壩
達馬拉超級集團 Swakop Navachab Karibib 大理石
石灰石、片岩、石英岩
烏薩科斯 Okonguarri(相當於阿蘭迪斯) 片岩,灰巖,石灰岩
Chuos 二硝石,鐵的形成
Nosib
Etusis 或同等物 arkosic 石英岩、meta-arkose、礫岩、石灰石、頁岩、片麻岩
達馬拉前地下室-Huab 變質複合體 片麻岩,小閃石

The Okonguarri Formation comprises a rhythmically interbedded sequence of limestone and meta-pelitic sediments (greywackes, schists, shales). This interbedded sequence of compositionally varying rocks introduces rheological contrasts (the way different rocks react to deformation) between lithologies or along lithological contacts which present favourable sites for potential mineralization (Figures 2 and 3).

奧孔瓜裏組由一系列有節奏地交織的石灰岩和重質沉積物(灰岩層、片岩和頁岩)組成。這種成分變化岩石的交錯序列在巖性之間或巖性接觸處引入了流變學對比(不同岩石對變形的反應方式),這爲潛在的礦化提供了有利的地點(圖 2 和 3)。

The post-tectonic intrusion of the PIC rupturing through the Damara Supergroup that has already undergone multiple deformation and metamorphic events provides lithological variation and structural complexity, defining characteristics of gold deposits seen in Namibia. The PIC appears to be situated at a zone of structural discontinuity indicated by the different regional fabric orientations of the Damaran stratigraphic units surrounding the complex as postulated by Siedner (1965)[i].

PIC破裂後的構造後入侵已經經歷了多次變形和變質事件的達馬拉超級群體,提供了巖性變化和結構複雜性,決定了納米比亞金礦的特徵。如西德納(1965)所假設的那樣,PIC似乎位於結構不連續的區域,該建築群周圍的達馬蘭地層單元的區域結構方向不同,這表明了這一點[我]

For more background information on the project, refer to News Release dated September 14, 2023.

有關該項目的更多背景信息,請參閱 2023 年 9 月 14 日的新聞稿。


Figure 3: Close-up of EPL 8711 with geological units over satellite imagery. Areas with no colour overlying the satellite imagery are covered by soil and/or calcrete. Coordinate System: WGS 84 UTM Zone 33 South; Units: Meters


圖 3:衛星影像上方的地質單位的 EPL 8711 特寫。衛星圖像上空沒有顏色的區域被土壤和/或鈣質混凝土覆蓋。座標系:WGS 84 UTM Zone 33 South;單位:米

About Antler Gold Inc.

關於 Antler Gold Inc.

Antler Gold Inc. is a Canadian listed mineral exploration company focused on organic royalty creation in Africa's Top-Ranked Jurisdictions. The Company continues to assess new regional opportunities with the aim of building a risk diversified business model that allows the Company to generate short and long-term income whilst providing stakeholders with exposure to potential multiple returns that are generated from the discovery process.

Antler Gold Inc. 是一家加拿大上市礦產勘探公司,專注於在非洲排名第一的司法管轄區創造有機特許權使用費。公司繼續評估新的區域機遇,目的是建立風險多元化的商業模式,使公司能夠產生短期和長期收入,同時爲利益相關者提供從發現過程中獲得的潛在多重回報的機會。

Qualified Person

合格人員

The technical and scientific information in this presentation has been reviewed and approved by Oliver Tors, B.Sc (Hons)., Exploration Manager of the Company, who is a registered Professional Natural Scientist (Pr.Sci.Nat. No. 120660) with the South African Council for Natural Scientific Professions (SACNASP) and a Qualified Person as defined by NI 43-101. Mr. Tors is an employee of Antler Gold Inc. and is not independent of the Company under NI 43-101.

本演示文稿中的技術和科學信息已獲得公司勘探經理、理學學士(榮譽)學位、註冊專業自然科學家(Pr.Sci.Nat)的審查和批准。編號爲120660),由南非自然科學專業委員會(SACNASP)和NI 43-101定義的合格人員。托爾斯先生是Antler Gold Inc.的員工,根據NI 43-101,他不獨立於公司。

Cautionary Statements

警示聲明

This press release may contain forward-looking information. This information is based on current expectations and assumptions (including assumptions relating to general economic and market conditions) that are subject to significant risks and uncertainties that are difficult to predict. Actual results may differ materially from results suggested in any forward-looking information. Antler Gold does not assume any obligation to update forward-looking information in this release, or to update the reasons why actual results could differ from those reflected in the forward-looking information unless and until required by securities laws applicable to Antler Gold. Additional information identifying risks and uncertainties is contained in the filings made by Antler Gold with Canadian securities regulators, which filings are available at .

本新聞稿可能包含前瞻性信息。這些信息基於當前的預期和假設(包括與總體經濟和市場狀況相關的假設),這些預期和假設存在難以預測的重大風險和不確定性。實際結果可能與任何前瞻性信息中建議的結果存在重大差異。除非適用於Antler Gold的證券法要求,否則Antler Gold不承擔任何義務更新本新聞稿中的前瞻性信息,也沒有義務更新實際業績可能與前瞻性信息中反映的結果不同的原因。識別風險和不確定性的其他信息包含在Antler Gold向加拿大證券監管機構提交的文件中,這些文件可在以下網址查閱。

Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.

多倫多證券交易所風險投資交易所及其監管服務提供商(該術語在多倫多證券交易所風險投資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。

For further information, please contact Christopher Drysdale, CEO of Antler Gold Inc., at +264 81 220 2439

欲了解更多信息,請致電 +264 81 220 2439 與 Antler Gold Inc. 首席執行官克里斯托弗·德賴斯代爾聯繫


[i]

[我]

Siedner, G., 1965. Structure and Evolution of the Paresis Igneous Complex, South West Africa. Transactions of the Geological Society of South Africa, pp. 177-206.

西德納,G.,1965 年。西南非洲帕雷西斯火成岩複合體的結構和演變。 南非地質學會會刊, 第 177-206 頁。

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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