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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 在纳米比亚的 Paresis 黄金项目启动黄金勘探计划
newsfile ·  02/05 10:48

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.(多伦多证券交易所股票代码:ANTL)(“Antler” 或 “公司”)欣然宣布,纳米比亚中北部的帕雷西斯金矿项目开始勘探工作。

Highlights

亮点

  • 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.
  • 帕雷西斯项目区域占地约21,000公顷,位于纳米比亚极具前景的 “黄金走廊” 内,该走廊是奥奇科托金矿(B2Gold)以及昂敦杜和尤里卡黄金项目(奥西诺资源)的所在地。
  • 在一个具有复杂变形和岩浆历史的地区进行的概念性项目提供了结构复杂性和岩性变化,这为与入侵相关的和造山风格的金矿床提供了潜力。
  • 优先目标区域:审查历史数据(地球化学和航空地球物理调查)、地区政府数据和卫星图像,可以确定岩性和结构目标区域并对其进行优先排序。

"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.

“我很高兴分享我们在Paresis黄金项目勘探工作的最新情况,这是纳米比亚著名的'黄金走廊'的一项重要举措。根据Antler的核心战略,公司打算通过盈利协议或类似协议寻找合适的合作伙伴来推进该项目,旨在最大限度地提高股东未来的发现收益。我感谢我们团队的奉献精神,我期待在不久的将来分享更多进展。” Antler Gold Inc.首席执行官克里斯托弗·德赖斯代尔说。

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.

勘探计划将分阶段推出,第一阶段是地质测绘和岩屑采样,然后是第二阶段的地球化学采样计划,视初始岩屑分析结果而定。Okonguarri和Karibib地层(均为Swakop集团)的潜在岩性单位位于许可区的下方,但是,该区域的大部分被土壤和钙质混凝土覆盖。

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).

奥孔瓜里组是奥奇科托金矿(B2Gold)和尤里卡金矿项目(奥西诺资源)的托管地层单元,而卡里比布组是达马拉地带中央区域各种金矿点(昂瓜蒂、戈德库佩、埃林迪)的金矿化场所,包括纳瓦查布金矿(QKR)(以及阿兰迪斯形成)(图 1、2 和 3)。

The Paresis Gold Project

帕雷西斯黄金项目

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).

帕雷西斯黄金项目目前由占地约21,000公顷的8711份独家勘探许可证(“EPL”)和另一份位于奥吉瓦龙戈镇和奥乔镇之间的EPL申请组成,距离纳米比亚中北部首都温得和克约290公里,位于达马拉造山带北部区域(新西兰)内。新西兰拥有众多矿床,包括奥奇科托金矿(B2Gold)、昂敦杜和尤里卡黄金项目(奥西诺资源)、奥坎扬德石墨矿床(北方石墨)和奥科鲁苏氟石矿等,证明了这种地质环境的肥沃性质(图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).

许可区域的露头暴露在中度至较高水平,包括来自前达马拉地下室、诺西布组和斯瓦科普组(下达马拉超级群)的岩石(图3,表1)。达马拉之前的地下室已紧紧地折叠成千米级的直立褶皱,大致向东西方向。达马拉序列受到了年轻的卡罗时代的白云岩堤坝和侏罗纪至白垩纪时代的帕雷西斯火成复合体(PIC)的干扰。

Table 1: NZ stratigraphy of the Paresis tenement.

表 1: 帕雷西斯物业单位的新西兰地层学.

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
顺序 小组 子组 形成 岩性学
麻疹火成复合物 (PIC) 双峰火山岩/挤出物、酸性和碱性侵入物
Karoo 超级群组 白云岩堤坝
达马拉超级集团 Swakop Navachab Karibib 大理石
石灰石、片岩、石英岩
乌萨科斯 Okonguarri(相当于阿兰迪斯) 片岩,灰岩,石灰岩
Chuos 二硝石,铁的形成
Nosib
Etusis 或同等物 arkosic 石英岩、meta-arkose、砾岩、石灰石、页岩、片麻岩
达马拉前地下室-Huab 变质复合体 片麻岩,小闪石

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).

奥孔瓜里组由一系列有节奏地交织的石灰岩和重质沉积物(灰岩层、片岩和页岩)组成。这种成分变化岩石的交错序列在岩性之间或岩性接触处引入了流变学对比(不同岩石对变形的反应方式),这为潜在的矿化提供了有利的地点(图 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破裂后的构造后入侵已经经历了多次变形和变质事件的达马拉超级群体,提供了岩性变化和结构复杂性,决定了纳米比亚金矿的特征。如西德纳(1965)所假设的那样,PIC似乎位于结构不连续的区域,该建筑群周围的达马兰地层单元的区域结构方向不同,这表明了这一点[我]

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

有关该项目的更多背景信息,请参阅 2023 年 9 月 14 日的新闻稿。


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


图 3:卫星影像上方的地质单位的 EPL 8711 特写。卫星图像上空没有颜色的区域被土壤和/或钙质混凝土覆盖。坐标系:WGS 84 UTM Zone 33 South;单位:米

About Antler Gold Inc.

关于 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. 是一家加拿大上市矿产勘探公司,专注于在非洲排名第一的司法管辖区创造有机特许权使用费。公司继续评估新的区域机遇,目的是建立风险多元化的商业模式,使公司能够产生短期和长期收入,同时为利益相关者提供从发现过程中获得的潜在多重回报的机会。

Qualified Person

合格人员

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.

本演示文稿中的技术和科学信息已获得公司勘探经理、理学学士(荣誉)学位、注册专业自然科学家(Pr.Sci.Nat)的审查和批准。编号为120660),由南非自然科学专业委员会(SACNASP)和NI 43-101定义的合格人员。托尔斯先生是Antler Gold Inc.的员工,根据NI 43-101,他不独立于公司。

Cautionary Statements

警示声明

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 .

本新闻稿可能包含前瞻性信息。这些信息基于当前的预期和假设(包括与总体经济和市场状况相关的假设),这些预期和假设存在难以预测的重大风险和不确定性。实际结果可能与任何前瞻性信息中建议的结果存在重大差异。除非适用于Antler Gold的证券法要求,否则Antler Gold不承担任何义务更新本新闻稿中的前瞻性信息,也没有义务更新实际业绩可能与前瞻性信息中反映的结果不同的原因。识别风险和不确定性的其他信息包含在Antler Gold向加拿大证券监管机构提交的文件中,这些文件可在以下网址查阅。

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.

多伦多证券交易所风险投资交易所及其监管服务提供商(该术语在多伦多证券交易所风险投资交易所的政策中定义)均不对本新闻稿的充分性或准确性承担责任。

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

欲了解更多信息,请致电 +264 81 220 2439 与 Antler Gold Inc. 首席执行官克里斯托弗·德赖斯代尔联系


[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.

西德纳,G.,1965 年。西南非洲帕雷西斯火成岩复合体的结构和演变。 南非地质学会会刊, 第 177-206 页。

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