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  • IsoEnergy在Larocque East項目進行ANt調查後，發現了六個新的高優先級鑽探目標。

IsoEnergy Generates Six New, High-Priority Drill Targets at Larocque East Project Following ANT Surveys

IsoEnergy Generates Six New, High-Priority Drill Targets at Larocque East Project Following ANT Surveys

IsoEnergy在Larocque East項目進行ANt調查後，發現了六個新的高優先級鑽探目標。
PR Newswire ·  08/15 19:00

TORONTO, Aug. 15, 2024 /PRNewswire/ - IsoEnergy Ltd. ("IsoEnergy" or the "Company") (TSX: ISO) (OTCQX: ISENF) is pleased to provide an update on its summer exploration program at the Larocque East Project (the "Project"), located in the eastern Athabasca Basin (Figure 1). The Company has successfully completed Ambient Noise Tomography ("ANT") surveys covering an additional 20 km2 constituting the remaining eastern extent of the property not previously covered. The surveys outlined six additional highly prospective target areas on strike of the Hurricane deposit to the east. To date, 23 diamond drill holes of the planned 27-hole program have been completed as part of the ongoing summer exploration program, totaling 9,660 meters, the results of which will be forthcoming on completion of the program anticipated in late August.

IsoEnergy有限公司（以下簡稱「公司」）（TSX：ISO）（OTCQX：ISENF）很榮幸地提供了Larocque East Project項目（以下簡稱「項目」）位於Athabasca Basin東部的夏季勘探計劃的更新（參見圖1）。公司已成功完成了周圍噪音層析成像（「ANT」）調查，涵蓋了20平方公里的面積，這是以前未曾覆蓋的東部物業的剩餘部分。該調查描繪出了六個高度前景性的目標區域，位於颶風礦牀向東的延伸上。截至目前，正在進行夏季勘探計劃的23個鑽孔中，已完成了計劃中的27個鑽孔中的9,660米，這些結果將在預計8月底完成的計劃完成之後公佈。

Figure 1 – Location map of the Hurricane deposit and IsoEnergy exploration projects in the eastern Athabasca Basin. (CNW Group/IsoEnergy Ltd.)
圖1-颶風礦牀和IsoEnergy在Athabasca盆地東部的勘探項目的位置圖。（CNW Group / IsoEnergy Ltd.）
Figure 2 – The Hurricane deposit footprint illustrating the close proximity of the three pre-discovery drill holes (KER-07, 11 & 12) and the IsoEnergy discovery drill hole LE18-01A within the ANT Anomaly (CNW Group/IsoEnergy Ltd.)
圖2-颶風礦牀足跡，顯示三個預發現鑽孔（KER-07，11和12）和IsoEnergy發現鑽孔LE18-01A與ANt異常之間的密切接觸。（CNW Group / IsoEnergy Ltd.）
Figure 3 – New ANT survey results from the eastern portion of the Larocque East Project illustrating six new target areas (E through to J). (CNW Group/IsoEnergy Ltd.)
圖3-Larocque East項目東部的新ANT調查結果，描繪了六個新的目標區域（E至J）。 （CNW Group / IsoEnergy Ltd.）
Figure 4 – Altered sandstone 12 to 20 metres above the unconformity in Target Area B (LE24-181, 269.0- 276.7m). The core is strongly bleached with intervals of desilicification, strong clay alteration (lower three rows) and local secondary hematite (patchy in upper two rows). Mineral spectroscopy results are pending. (CNW Group/IsoEnergy Ltd.)
圖4-目標區域b中不整合上方12至20米的改變砂岩（LE24-181，269.0-276.7m）。核心區域受強烈漂白，存在脫硅，強烈粘土化 alteration（下三行）以及局部二次赤鐵礦（上兩行中的斑狀）。礦物光譜學結果正在等待。（CNW Group / IsoEnergy Ltd.）
Figure 5 – Altered sandstone 17 to 35 metres above the unconformity in Target Area B (LE24-165, 269.7-288.1m). The core is strongly bleached with intervals of desilicification, strong clay alteration (mostly in the lower six rows) and local secondary hematite (some of the hematite in rows two to four). Mineral spectroscopy classifies the clay as 100% illite. (CNW Group/IsoEnergy Ltd.)
圖5-目標區域b上方17至35米的改變砂岩（LE24-165，269.7-288.1m）。核心區域受強烈漂白，存在脫硅，強烈粘土化 alteration（主要在下六行中）以及局部二次赤鐵礦（第二至第四行中的某些赤鐵礦）。礦物光譜法將粘土分類爲100％的滑石。（CNW Group / IsoEnergy Ltd.）
Figure 6 – Altered sandstone 35 to 55 metres above the unconformity in Target Area A (LE24-158, 242.4-263m). The core is pervasively bleached and exhibits limonite staining in strongly clay altered and desilicified rubbly intervals that make up about 50% of the photographed core. Mineral spectroscopy indicates an illite – dickite clay species mixture. (CNW Group/IsoEnergy Ltd.)
圖6-目標區域A中不整合上方35至55米的改變砂岩（LE24-158，242.4-263m）。核心區域普遍漂白，呈現鎘鐵礦染色的強烈粘土化 alteration 和脫硅灰暗顆粒狀間隙，延伸約50％的攝影核心。礦物光譜學表明一種滑石-迪凱特混合粘土礦。（CNW Group / IsoEnergy Ltd.）
Figure 7 – Altered sandstone 10 to 30 metres above the unconformity in Target Area D (LE24-172, 260.7- 278.7m). The core is moderately to strongly bleached with patches of preserved purple diagenetic hematite. Much of the photographed interval is rubbly and desilicified, with local intervals of intense clay alteration and patchy secondary hematite. Mineral spectroscopy indicates an illite – dickite clay species mixture. (CNW Group/IsoEnergy Ltd.)
圖7-目標區域D不整合上方10至30米的改變砂岩（LE24-172，260.7-278.7m）。 核心區域強烈漂白，存有保留的紫色成巖赤鐵礦。攝影的間隙大部分是粗糙的脫硅灰暗顆粒狀，有局部強烈粘土化 alteration和斑狀二次赤鐵礦。礦物光譜學結果顯示一種滑石-迪凱特混合粘土礦。（CNW Group / IsoEnergy Ltd.）
Figure 8 – Chloritized basement gneisses 5 to 10 metres below the unconformity in Target Area D (LE24-176, 283.4-289.5m). The mineral spectroscopy classification is dominated by sudoite (chlorite) with lesser illite. (CNW Group/IsoEnergy Ltd.)
圖8-目標區域D不整合下面5至10米的氯化基底片麻岩（LE24-176，283.4-289.5m）。礦物光譜法分類以Chloritized基底片麻岩爲主，較少爲滑石。 （CNW Group / IsoEnergy Ltd.）

譯文內容由第三人軟體翻譯。


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