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Metal Energy Provides Results From SourceRock Project

Metal Energy Provides Results From SourceRock Project

金属能源提供了 SourceRock 项目的结果
newsfile ·  03/26 06:00

Toronto, Ontario--(Newsfile Corp. - March 26, 2024) - Metal Energy Corp. (TSXV: MERG) (OTCQB: MEEEF) (the "Company" or "Metal Energy") is pleased to release the brine and lithogeochemical results (Tables 1 & 2) from two brine reservoirs intersected in the Company's first drill hole (SR-24-01) at the SourceRock project ("SourceRock" or the "Project") near Thunder Bay, Ontario.

安大略省多伦多--(Newsfile Corp.,2024年3月26日)——金属能源公司(TSXV:MERG)(场外交易代码:MEEEF)(the”公司“或”金属能量“) 很高兴公布该公司在SourceRock项目的第一个钻孔(SR-24-01)中相交的两个盐水储层的盐水和岩石地球化学结果(表1和表2)(”源岩石“或者”项目“)在安大略省桑德贝附近。

The brine results (Table 1) identified Total Dissolved Solids ("TDS") concentrations increasing with depth and seem to correlate well with rock types. Importantly, concentrations of sodium (Na) and potassium (K), including calcium (Ca), increase almost exponentially with depth. Lithium (Li) tends to follow Na and K, specifically. The highest brine results, up to 6.0% TDS, were intersected within a clean sandstone unit at the base of the sedimentary formations. Lithium bearing brines are globally associated with chloride-rich fluids. Additional analysis of the brines determined over 90% of the inorganic anions within the calcareous mudstone-rich units as chlorides (Cl), not sulphates, carbonates, nitrites or nitrates, and over 97% chlorides in the sandstone-rich units. These inorganic results demonstrate the right type of brines are present on the Project.

盐水结果(表 1)确定了溶解固体总量(”TDS“) 浓度随着深度的增加而增加,似乎与岩石类型密切相关。重要的是,钠(Na)和钾(K),包括钙(Ca)的浓度几乎随深度呈指数级增长。具体而言,锂(Li)倾向于遵循钠和钾。在沉积层底部的干净砂岩单元内相交时,盐水结果最高,TDS 高达 6.0%。含锂盐水在全球范围内都与富含氯化物的液体有关。对盐水的进一步分析确定,富含钙质泥石的单元中90%以上的无机阴离子是氯化物(Cl),而不是硫酸盐、碳酸盐、亚硝酸盐或硝酸盐,富含砂岩的单元中超过97%的氯化物。这些无机结果表明,该项目中存在正确类型的盐水。

The lithogeochemical results of the host rock formations (Table 2) show the calcareous mudstones are enriched with calcium (Ca) and magnesium (Mg) which is expected due to high concentrations of gypsum in the drill core. The sandstones, however, are mostly quartz-rich and are generally devoid of elemental constituents. Historic drill hole BSW-06-04A located 5km to the north (Figure 1) intersected salt beds within the sandstone unit of the sedimentary formation, however, drill hole SR24-01 did not intersect similar results.

主岩层的岩石地球化学结果(表 2)显示,钙质泥岩富含钙(Ca)和镁(Mg),这是由于钻芯中石膏浓度高所致。但是,砂岩大多富含石英,通常不含元素成分。位于北 5 公里处的历史钻孔 BSW-06-04A(图 1)与沉积层砂岩单元内的盐床相交,但是,SR24-01 钻孔没有碰到类似的结果。

Careful analysis of the brine and rock results from recent and historic drill holes on the Project suggests SR-24-01 is on the edge of a large mature halite salar (i.e., salt flat) (Figure 2). A typical sedimentary deposition model for a salar includes a central halite (NaCl) nucleus that grades outward in concentric sequences including fine-grained clastic rocks, such as sandstone, and marginal marine rocks enriched with gypsum and/or carbonate, such as calcareous mudstones.

对该项目最近和历史钻孔的盐水和岩石结果的仔细分析表明,SR-24-01 位于大型成熟盐岩(即盐滩)的边缘(即盐滩)(图 2)。盐岩的典型沉积沉积模型包括中心盐岩(NaCl)核,该核按同心顺序向外分级,包括砂岩等细颗粒碎屑岩和富含石膏和/或碳酸盐的边缘海洋岩石,例如钙质泥岩。

"Our next step is to map the subsurface geology with a geophysical survey to better determine the possible location of a central halite nucleus as the brine results from SR-24-01 clearly indicate a positive correlation between increased Na with increased Li," commented James Sykes, CEO of Metal Energy.

金属能源首席执行官詹姆斯·赛克斯评论说:“我们的下一步是通过地球物理调查绘制地下地质图,以更好地确定中心盐岩核的可能位置,因为 SR-24-01 的盐水结果清楚地表明,钠的增加与锂的增加之间呈正相关关系。”

The Company plans to follow-up the details of this news release and drill hole results with an interpretative presentation in the future.

该公司计划将来通过解释性演示来跟踪本新闻稿的细节和钻孔结果。

SourceRock Drill Program Details

SourceRock 钻探计划详情

Drill hole SR-24-01 was completed down to 542 m. Detailed core logging plus a suite of downhole geophysical surveys were used to assess the brines and rock characteristics within the sedimentary units. Brine sampling was performed at specific depths to determine brine constituents from sedimentary horizons with the highest fluid conductivity responses, as well as over large intervals to determine background brine constituent levels.

SR-24-01 钻孔已完成,深度可达 542 米。详细的岩心测井和一系列井下地球物理调查用于评估沉积单元内的盐水和岩石特征。盐水采样是在特定深度进行的,以确定具有最高流体电导率响应的沉积层中的盐水成分,并进行了较长的时间间隔以确定背景盐水成分含量。

About the SourceRock Lithium Brine Project

关于 SourceRock 锂盐水项目

SourceRock is highly prospective for lithium brines in the Thunder Bay-Nipigon area of northwestern Ontario. The Project is exceptionally large, covering 915 square kilometres (91,477 ha.) within an area measuring approximately 10 to 20 km wide by 95 km long (Figure 1) of the Proterozoic Sibley sedimentary basin, a size equivalent to the World's second largest lithium producing jurisdiction; Chile's Salar de Atacama's Central Salt Belt.

SourceRock在安大略省西北部的桑德贝-尼皮贡地区对锂盐水的开发前景非常有希望。该项目规模极大,占地915平方千米(91,477公顷),位于元古代西布利沉积盆地宽约10至20千米,长95千米(图1)的区域内,面积相当于世界第二大锂生产管辖区:智利的阿塔卡马盐带。

The Project has excellent access to infrastructure and capacity that has supported previous exploration programs and mine development, including year-round highway, railroad, and seaport access, with power and natural gas lines crossing the Project.

该项目拥有良好的基础设施和容量,为先前的勘探计划和矿山开发提供了支持,包括全年通用的公路、铁路和海港通道,以及横穿该项目的电力和天然气管线。

For the latest videos from Metal Energy and other Ore Group companies, subscribe to our YouTube channel: youtube.com/@theoregroup

如需了解来自金属能源和其他矿石集团公司的最新视频,请订阅我们的 YouTube 频道: youtube.com/ @theoregroup

About Metal Energy Corp.

关于金属能源公司

Metal Energy is a battery metal exploration company with two projects in politically stable Canadian jurisdictions: Manibridge (Ni-Cu-Co-PGE) in Manitoba, and SourceRock (Li-Na-K) in Ontario. The Manibridge Project is 85% owned by Metal Energy and 15% owned by Mistango River Resources Inc. (CSE: MIS). SourceRock is subject to earn-in agreement where the Company can acquire 100% exploration rights to the project.

金属能源是一家电池金属勘探公司,在政治稳定的加拿大司法管辖区有两个项目:曼尼托巴省的Manibridge(NI-CU-Co-PGE)和安大略省的SourceRock(Li-Na-K)。Manibridge项目由金属能源公司持有85%的股权,米斯坦戈河资源公司(CSE:MIS)拥有15%的股权。SourceRock受盈利协议的约束,根据该协议,公司可以获得该项目的100%的勘探权。

QP Statement

QP 声明

The technical information contained in this news release has been reviewed and approved by Mike Sweeny, P.Geo., Technical Advisor for Metal Energy, and a Qualified Person as defined in "National Instrument 43-101, Standards of Disclosure for Mineral Projects."

本新闻稿中包含的技术信息已经过金属能源技术顾问Mike Sweeny的审查和批准,P.Geo.,以及 “National Instrument 43-101,矿业项目披露标准” 中定义的合格人士。

For further information, please contact:

欲了解更多信息,请联系:

Metal Energy Corp.
MERG on the TSXV
info@metalenergy.ca

金属能源公司
在多伦多证券交易所上市 MERG
info@metalenergy.ca

James Sykes, CEO
jsykes@oregroup.ca
306-221-8717

首席执行官詹姆斯·赛克斯
jsykes@oregroup.ca
306-221-8717

Reader Advisory

读者咨询

Certain information set forth in this news release contains forward-looking statements or information ("forward-looking ‎statements"), including details about the business of the Company. By their nature, forward-looking statements are subject to numerous risks ‎and uncertainties, some of which are beyond the Company's control, including the impact of general economic conditions, ‎industry conditions, volatility of commodity prices, currency fluctuations, environmental risks, operational risks, competition from ‎other industry participants, stock market volatility. Although the ‎Company believes that the expectations in its forward-looking statements are reasonable, its forward-looking statements have ‎been based on factors and assumptions concerning future events which may prove to be inaccurate. Those factors and ‎assumptions are based upon currently available information. Such statements are subject to known and unknown risks, ‎uncertainties and other factors that could influence actual results or events and cause actual results or events to differ materially ‎from those stated, anticipated or implied in the forward-looking statements. Accordingly, readers are cautioned not to place undue ‎reliance on the forward-looking statements, as no assurance can be provided as to future results, levels of activity or achievements. ‎Risks, uncertainties, material assumptions and other factors that could affect actual results are discussed in our public disclosure ‎documents available at including the Filing Statement dated November 15, 2021. Furthermore, the forward-looking statements contained in this document are made as of ‎the date of this document and, except as required by applicable law, the Company does not undertake any obligation to publicly ‎update or to revise any of the included forward-looking statements, whether as a result of new information, future events or ‎otherwise. The forward-looking statements contained in this document are expressly qualified by this cautionary statement.‎

本新闻稿中列出的某些信息包含前瞻性陈述或信息(”前瞻性陈述“),包括有关公司业务的详细信息。就其性质而言,前瞻性陈述受许多风险和不确定性的影响,其中一些是公司无法控制的,包括总体经济状况、行业状况、大宗商品价格波动、货币波动、环境风险、运营风险、来自其他行业参与者的竞争、股市波动的影响。尽管公司认为其前瞻性陈述中的预期是合理的,但其前瞻性陈述基于有关未来事件的因素和假设,这些因素和假设可能被证明是不准确的。这些因素和假设以现有信息为基础。此类陈述受已知和未知的风险、不确定性和其他因素的影响,这些因素可能会影响实际业绩或事件,并导致实际业绩或事件与前瞻性陈述中陈述、预期或暗示的结果或事件存在重大差异。因此,提醒读者不要过分依赖前瞻性陈述,因为无法保证未来的业绩、活动水平或成就。我们的公开披露文件中讨论了风险、不确定性、重大假设和其他可能影响实际业绩的因素,网址为 包括日期为2021年11月15日的申报声明。此外,本文件中包含的前瞻性陈述自本文件发布之日起作出,除非适用法律要求,否则公司不承担任何公开更新或修改所含任何前瞻性陈述的义务,无论是由于新信息、未来事件还是其他原因。本警示声明对本文件中包含的前瞻性陈述进行了明确限定。

Neither the TSX Venture Exchange Inc. 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.

TSX Venture Exchange Inc. 及其监管服务提供商(该术语在多伦多证券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。

TABLE 1 — Brine (fluid) results

表 1 — 盐水(液体)结果

DDH Reservoir Lithology From To Interval Li (mg/L) Ca (mg/L) Fe (mg/L) K (mg/L) Mg (mg/L) Na (mg/L) TDS (mg/L) Na/TDS
SR24-01 Upper Calcareous mudstone/siltstone 151.90 159.40 7.50 0.0 37 17 5.6 5.7 570 671 85%
Lower Calcareous mudstone/sandstone 484.90 492.40 7.50 0.0 43 120 7.8 5.6 800 985 81%
Lower Sandstone/calcareous mudstone 496.40 503.90 7.50 0.3 340 200 59 11 7700 8331 92%
Lower Sandstone 508.90 516.40 7.50 2.3 2200 240 450 43 57000 59980 95%
DDH 水库 岩性学 来自 间隔 锂 (mg/L) 钙 (mg/L) 铁 (mg/L) K (mg/L) 镁 (mg/L) 钠 (mg/L) TDS (mg/L) NA/TDS
SR24-01 上部 钙质泥岩/粉砂岩 151.90 159.40 7.50 0.0 37 17 5.6 5.7 570 671 85%
降低 钙质泥岩/砂岩 484.90 492.40 7.50 0.0 43 120 7.8 5.6 800 985 81%
降低 砂岩/钙质泥岩 496.40 503.90 7.50 0.3 340 200 59 11 7700 8331 92%
降低 砂岩 508.90 516.40 7.50 2.3 2200 240 450 43 57000 59980 95%


NOTES:
1. 1.0 mg/L = 1.0 ppm


笔记:
1. 1.0 mg/L = 1.0 ppm

TABLE 2 — Lithogeochemical (rock) Composite results

表 2 — 岩石地球化学(岩石)综合结果

DDH Reservoir Lithology From To Interval Li (ppm) CaO (%) Fe2O3 (%) K2O (%) MgO (%) Na2O (%)
SR24-01 Upper Calcareous mudstone/siltstone 150.24 197.63 47.39 121.6 20.1 2.4 1.1 23.1 1.4
Lower Calcareous mudstone/sandstone 473.62 494.62 21.00 122.3 15.5 2.7 2.5 19.8 1.4
Lower Sandstone/calcareous mudstone 494.62 514.62 20.00 35.0 2.6 0.8 0.8 4.2 1.3
Lower Sandstone 514.62 520.32 5.70 6.9 0.2 0.2 0.1 0.3 0.3
DDH 水库 岩性学 来自 间隔 李 (ppm) 氧化钙 (%) 2O3 (%) K2O (%) 氧化镁 (%) 2O (%)
SR24-01 上部 钙质泥岩/粉砂岩 150.24 197.63 47.39 121.6 20.1 2.4 1.1 23.1 1.4
降低 钙质泥岩/砂岩 473.62 494.62 21.00 122.3 15.5 2.7 2.5 19.8 1.4
降低 砂岩/钙质泥岩 494.62 514.62 20.00 35.0 2.6 0.8 0.8 4.2 1.3
降低 砂岩 514.62 520.32 5.70 6.9 0.2 0.2 0.1 0.3 0.3


NOTES:
1. Composite summary results were restricted to similar lithologies and did not include cutoff grades or dilution factor
2. 1.0% = 10,000 ppm


笔记:
1。综合汇总结果仅限于相似的岩性,不包括截止等级或稀释系数
2. 1.0% = 10,000 ppm

TABLE 3 — Drill hole collar coordinates

表 3 — 钻孔环坐标

DDH East North Elevation Azimuth Dip EOH
SR24-01 367,982 5,459,095 279 270 -80 542
DDH 东方 北方 海拔 方位角 哎哟
SR24-01 367,982 5,459,095 279 270 -80 542

NOTES: East and North units are metres using NAD83 datum, UTM Zone 16N
Elevation is recorded as "metres above sea level"
EOH = End of hole, measured in metres

注意:使用 NAD83 基准时,东部和北部的单位均为米,UTM 区域 16N
海拔记录为 “海拔米”
EOH = 洞底,以米为单位测量

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