Metal Energy Provides Results From SourceRock Project
Metal Energy Provides Results From SourceRock Project
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.
安大略省多倫多--(Newsfile Corp.,2024年3月26日)——金屬能源公司(TSXV:MERG)(場外交易代碼:MEEEF)(the”公司“或”金屬能量“) 很高興公佈該公司在SourceRock項目的第一個鑽孔(SR-24-01)中相交的兩個鹽水儲層的鹽水和岩石地球化學結果(表1和表2)(”源岩石“或者”項目“)在安大略省桑德貝附近。
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.
鹽水結果(表 1)確定了溶解固體總量(”TDS“) 濃度隨着深度的增加而增加,似乎與岩石類型密切相關。重要的是,鈉(Na)和鉀(K),包括鈣(Ca)的濃度幾乎隨深度呈指數級增長。具體而言,鋰(Li)傾向於遵循鈉和鉀。在沉積層底部的乾淨砂岩單元內相交時,鹽水結果最高,TDS 高達 6.0%。含鋰鹽水在全球範圍內都與富含氯化物的液體有關。對鹽水的進一步分析確定,富含鈣質泥石的單元中90%以上的無機陰離子是氯化物(Cl),而不是硫酸鹽、碳酸鹽、亞硝酸鹽或硝酸鹽,富含砂岩的單元中超過97%的氯化物。這些無機結果表明,該項目中存在正確類型的鹽水。
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.
主岩層的岩石地球化學結果(表 2)顯示,鈣質泥岩富含鈣(Ca)和鎂(Mg),這是由於鑽芯中石膏濃度高所致。但是,砂岩大多富含石英,通常不含元素成分。位於北 5 公里處的歷史鑽孔 BSW-06-04A(圖 1)與沉積層砂岩單元內的鹽牀相交,但是,SR24-01 鑽孔沒有碰到類似的結果。
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.
對該項目最近和歷史鑽孔的鹽水和岩石結果的仔細分析表明,SR-24-01 位於大型成熟鹽巖(即鹽灘)的邊緣(即鹽灘)(圖 2)。鹽巖的典型沉積沉積模型包括中心鹽巖(NaCl)核,該核按同心順序向外分級,包括砂岩等細顆粒碎屑岩和富含石膏和/或碳酸鹽的邊緣海洋岩石,例如鈣質泥岩。
"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.
金屬能源首席執行官詹姆斯·賽克斯評論說:“我們的下一步是通過地球物理調查繪製地下地質圖,以更好地確定中心鹽巖核的可能位置,因爲 SR-24-01 的鹽水結果清楚地表明,鈉的增加與鋰的增加之間呈正相關關係。”
The Company plans to follow-up the details of this news release and drill hole results with an interpretative presentation in the future.
該公司計劃將來通過解釋性演示來跟蹤本新聞稿的細節和鑽孔結果。
SourceRock Drill Program Details
SourceRock 鑽探計劃詳情
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 鑽孔已完成,深度可達 542 米。詳細的岩心測井和一系列井下地球物理調查用於評估沉積單元內的鹽水和岩石特徵。鹽水採樣是在特定深度進行的,以確定具有最高流體電導率響應的沉積層中的鹽水成分,並進行了較長的時間間隔以確定背景鹽水成分含量。
About the SourceRock Lithium Brine Project
關於 SourceRock 鋰鹽水項目
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貝-尼皮貢地區對鋰鹽水的開發前景非常有希望。該項目規模極大,佔地915平方千米(91,477公頃),位於元古代西布利沉積盆地寬約10至20千米,長95千米(圖1)的區域內,面積相當於世界第二大鋰生產管轄區:智利的阿塔卡馬鹽帶。
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.
該項目擁有良好的基礎設施和容量,爲先前的勘探計劃和礦山開發提供了支持,包括全年通用的公路、鐵路和海港通道,以及橫穿該項目的電力和天然氣管線。
For the latest videos from Metal Energy and other Ore Group companies, subscribe to our YouTube channel: youtube.com/@theoregroup
如需了解來自金屬能源和其他礦石集團公司的最新視頻,請訂閱我們的 YouTube 頻道: youtube.com/ @theoregroup
About Metal Energy Corp.
關於金屬能源公司
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.
金屬能源是一家電池金屬勘探公司,在政治穩定的加拿大司法管轄區有兩個項目:曼尼托巴省的Manibridge(NI-CU-Co-PGE)和安大略省的SourceRock(Li-Na-K)。Manibridge項目由金屬能源公司持有85%的股權,米斯坦戈河資源公司(CSE:MIS)擁有15%的股權。SourceRock受盈利協議的約束,根據該協議,公司可以獲得該項目的100%的勘探權。
QP Statement
QP 聲明
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."
本新聞稿中包含的技術信息已經過金屬能源技術顧問Mike Sweeny的審查和批准,P.Geo.,以及 “National Instrument 43-101,礦業項目披露標準” 中定義的合格人士。
For further information, please contact:
欲了解更多信息,請聯繫:
Metal Energy Corp.
MERG on the TSXV
info@metalenergy.ca
金屬能源公司
在多倫多證券交易所上市 MERG
info@metalenergy.ca
James Sykes, CEO
jsykes@oregroup.ca
306-221-8717
首席執行官詹姆斯·賽克斯
jsykes@oregroup.ca
306-221-8717
Reader Advisory
讀者諮詢
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.
本新聞稿中列出的某些信息包含前瞻性陳述或信息(”前瞻性陳述“),包括有關公司業務的詳細信息。就其性質而言,前瞻性陳述受許多風險和不確定性的影響,其中一些是公司無法控制的,包括總體經濟狀況、行業狀況、大宗商品價格波動、貨幣波動、環境風險、運營風險、來自其他行業參與者的競爭、股市波動的影響。儘管公司認爲其前瞻性陳述中的預期是合理的,但其前瞻性陳述基於有關未來事件的因素和假設,這些因素和假設可能被證明是不準確的。這些因素和假設以現有信息爲基礎。此類陳述受已知和未知的風險、不確定性和其他因素的影響,這些因素可能會影響實際業績或事件,並導致實際業績或事件與前瞻性陳述中陳述、預期或暗示的結果或事件存在重大差異。因此,提醒讀者不要過分依賴前瞻性陳述,因爲無法保證未來的業績、活動水平或成就。我們的公開披露文件中討論了風險、不確定性、重大假設和其他可能影響實際業績的因素,網址爲 包括日期爲2021年11月15日的申報聲明。此外,本文件中包含的前瞻性陳述自本文件發佈之日起作出,除非適用法律要求,否則公司不承擔任何公開更新或修改所含任何前瞻性陳述的義務,無論是由於新信息、未來事件還是其他原因。本警示聲明對本文件中包含的前瞻性陳述進行了明確限定。
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. 及其監管服務提供商(該術語在多倫多證券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。
TABLE 1 — Brine (fluid) results
表 1 — 鹽水(液體)結果
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 | 水庫 | 巖性學 | 來自 | 到 | 間隔 | 鋰 (mg/L) | 鈣 (mg/L) | 鐵 (mg/L) | K (mg/L) | 鎂 (mg/L) | 鈉 (mg/L) | TDS (mg/L) | NA/TDS |
SR24-01 | 上部 | 鈣質泥岩/粉砂岩 | 151.90 | 159.40 | 7.50 | 0.0 | 37 | 17 | 5.6 | 5.7 | 570 | 671 | 85% |
降低 | 鈣質泥岩/砂岩 | 484.90 | 492.40 | 7.50 | 0.0 | 43 | 120 | 7.8 | 5.6 | 800 | 985 | 81% | |
降低 | 砂岩/鈣質泥岩 | 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
筆記:
1. 1.0 mg/L = 1.0 ppm
TABLE 2 — Lithogeochemical (rock) Composite results
表 2 — 岩石地球化學(岩石)綜合結果
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 | 水庫 | 巖性學 | 來自 | 到 | 間隔 | 李 (ppm) | 氧化鈣 (%) | 鐵2O3 (%) | K2O (%) | 氧化鎂 (%) | 娜2O (%) |
SR24-01 | 上部 | 鈣質泥岩/粉砂岩 | 150.24 | 197.63 | 47.39 | 121.6 | 20.1 | 2.4 | 1.1 | 23.1 | 1.4 |
降低 | 鈣質泥岩/砂岩 | 473.62 | 494.62 | 21.00 | 122.3 | 15.5 | 2.7 | 2.5 | 19.8 | 1.4 | |
降低 | 砂岩/鈣質泥岩 | 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
筆記:
1。綜合彙總結果僅限於相似的巖性,不包括截止等級或稀釋係數
2. 1.0% = 10,000 ppm
TABLE 3 — Drill hole collar coordinates
表 3 — 鑽孔環座標
DDH | East | North | Elevation | Azimuth | Dip | EOH |
SR24-01 | 367,982 | 5,459,095 | 279 | 270 | -80 | 542 |
DDH | 東方 | 北方 | 海拔 | 方位角 | 浸 | 哎喲 |
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 基準時,東部和北部的單位均爲米,UTM 區域 16N
海拔記錄爲 “海拔米”
EOH = 洞底,以米爲單位測量
譯文內容由第三人軟體翻譯。