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Lithium One Identifies LCT Enrichment Trend at Two Properties in James Bay, Quebec

Lithium One Identifies LCT Enrichment Trend at Two Properties in James Bay, Quebec

Lithium One确定了魁北克詹姆斯湾两处房产的LCT浓缩趋势
newsfile ·  2023/11/07 07:20

Vancouver, British Columbia--(Newsfile Corp. - November 7, 2023) - Lithium One Metals Inc. (TSXV: LONE) (FSE: H490) (OTCQB: LOMEF) (the "Company" or "Lithium One") is pleased to announce results from phase one of its exploration campaign in the James Bay lithium district, Quebec. A systematic sampling and mapping program has been completed at Highway, Taycan, Bus and Bugatti properties with initial results highlighting an elevated trend of lithium-cesium-tantalum (LCT) pegmatite indicators at Highway and Bus properties. The newly identified trend will be prioritized for drill testing in the upcoming, multi-project drill program.

不列颠哥伦比亚省温哥华--(Newsfile Corp.,2023 年 11 月 7 日)-Lithium One Metals Inc.(多伦多证券交易所股票代码:LONE)(FSE:H490)(场外交易代码:LOMEF)(the”公司“或”锂一号“)很高兴地宣布其在魁北克詹姆斯湾锂区的第一阶段勘探活动的结果。Highway、Taycan、Bus和Bugatti物业的系统采样和测绘计划已经完成,初步结果显示,公路和公共汽车物业中锂-铯-钽(LCT)伟晶岩指标呈上升趋势。在即将到来的多项目钻探计划中,新确定的趋势将优先用于钻探测试。

Highlights

亮点

  • LCT Enrichment Trend at Highway and Bus Properties. Abundant pegmatites were mapped on all four properties with anomalous Li, Cs, Ta, and Rb results returned in initial samples from Highway and Bus. These results highlight a new trend of elevated LCT pegmatite indicator elements, which will be the focus of the Company's next phase of exploration.
  • 公路和公共汽车地产的LCT浓缩趋势。 在所有四个特性上绘制了丰富的伟晶岩,在公路和公共汽车的初始样本中返回了异常的锂、碳、钽和硼结果。这些结果凸显了LCT伟晶岩指标元素升高的新趋势,这将是该公司下一阶段勘探的重点。
  • Drill Program to Commence in early Q1, 2024. Lithium One has identified several target areas for drill testing and permit applications have been submitted.
  • 钻探计划将于2024年第一季度初开始。 Lithium One已经确定了钻探测试的几个目标区域,并且已经提交了许可证申请。

Figure 1. Lithium One's Highway, Bus, Taycan and Bugatti Lithium Properties in the James Bay region of Quebec. Initial sample results at Highway and Bus properties define a new elevated trend of indicator elements indicative of LCT pegmatite prospectivity.

图 1。 Lithium One位于魁北克詹姆斯湾地区的公路、巴士、Taycan和布加迪锂业公司。公路和公共汽车地产的初步样本结果定义了表明LCT伟晶岩前景的指标元素的新上升趋势。

Figure 2. Results for Li, Cs, Rb, Ta from surface sampling at the Highway Lithium Property.

图 2。 高速公路锂矿地表面采样得出的锂、碳、硼、钽的结果。

Figure 3. Location of mapped pegmatite outcrops at the Highway Lithium Property showing the trend of elevated LCT pegmatite indicator elements.

图 3。 公路锂地产中绘制的伟晶岩露头位置显示了LCT伟晶岩指示元素升高的趋势。

Figure 4. Results for Li, Cs, Rb, Ta from surface sampling at the Bus Lithium Property.

图 4。 从巴士锂矿物业的表面采样得出的锂、碳、铅、钽的结果。

Figure 5. Location of mapped pegmatite outcrops at the Bus Lithium Property showing the trend of elevated LCT pegmatite indicator elements.

图 5. Bus Lithium Property 中绘制的伟晶岩露头位置显示 LCT 伟晶岩指示元素升高的趋势。

Results Discussion

结果讨论

The Highway property returned 8 samples with assays above 150 ppm Li, with the highest being 539 ppm Li in sample 267199. A total of 47 samples returned anomalous amounts of one or more marker element including lithium (>150 ppm), cesium (>50 ppm), rubidium (>900 ppm), and tantalum (>20 ppm). The highest concentration of anomalous results is associated with observed lepidolite in the field.

公路物业返回了8份样本,其化验结果高于150 ppm Li,其中267199样本中最高的为539 ppm Li。共有47个样本返回了异常数量的一种或多种标记元素,包括锂(>150 ppm)、(>50 ppm)、铑(>900 ppm)和钽(>20 ppm)。异常结果的最高浓度与野外观测到的锂云母有关。

On the Bus property, 9 of 20 samples collected returned anomalies in marker elements. Samples 710588 and 710894 returned 155 ppm Li and 182 ppm Li respectively.

在 Bus 属性上,收集的 20 个样本中有 9 个返回了标记元素中的异常。710588 和 710894 样本分别返回了 155 ppm Li 和 182 ppm Li。

The anomalous samples collected are spatially correlated, identifying the enrichment trends for both properties. The enrichment trends identified in surface sampling are indicative of LCT pegmatite prospectivity and will be followed up on with drilling in 2024.

收集的异常样本在空间上相互关联,确定了这两种特性的富集趋势。地表采样中确定的富集趋势表明了LCT伟晶岩的前景,并将于2024年继续进行钻探。

Table 1. Results and highlights from the Highway Lithium Property.

表 1。 公路锂地产的结果和亮点。

Sample # Lithology Cs (ppm) Li (ppm) Rb (ppm) Ta (ppm)
234798 Pegmatite 26.3 96 653 26
267083 Pegmatite 53.9 28 342 22.3
267175 Pegmatite 131 222 951 56
267176 Pegmatite 269 52 2000 14
267177 Pegmatite 204 123 1590 40.2
267178 Pegmatite 207 43 1720 45.6
267179 Pegmatite 254 107 1910 24.6
267180 Pegmatite 75.1 138 590 24.8
267181 Pegmatite 109 62 1440 7.8
267182 Pegmatite 113 61 1500 8.3
267183 Pegmatite 184 65 1450 22.8
267184 Pegmatite 228 99 1820 92.8
267185 Pegmatite 124 45 1260 15
267186 Pegmatite 37.8 99 334 22.2
267188 Pegmatite 114 50 1230 10
267189 Pegmatite 136 48 1470 9.9
267190 Pegmatite 74.9 212 700 52.8
267191 Pegmatite 30.8 94 291 27.6
267192 Pegmatite 59.1 73 388 36.6
267193 Pegmatite 116 85 1020 20.4
267194 Pegmatite 16.2 79 103 22.6
267198 Pegmatite 9.7 103 285 23.7
267199 Pegmatite 102 539 1580 213
267200 Pegmatite 25.7 184 421 470
267388 Pegmatite 125 72 464 34.1
267389 Pegmatite 124 165 863 41.7
267390 Pegmatite 6.9 36 46 35.6
267391 Pegmatite 11.1 37 35 36.6
267393 Pegmatite 8 30 42 37.4
267394 Pegmatite 49.6 36 410 25.4
267395 Pegmatite 18 203 84 33.1
267396 Pegmatite 27.2 76 114 31.1
267397 Pegmatite 14.7 249 68 20.2
267398 Pegmatite 10.8 235 57 20.6
267400 Pegmatite 346 23 1620 7.2
267428 Pegmatite 237 28 2090 11.9
726881 Pegmatite 13.7 -10 602 29.3
示例 # 岩性学 Cs (ppm) 李 (ppm) Rb (ppm) Ta (ppm)
234798 伟晶岩 26.3 96 653 26
267083 伟晶岩 53.9 28 342 22.3
267175 伟晶岩 131 222 951 56
267176 伟晶岩 269 52 2000 14
267177 伟晶岩 204 123 1590 40.2
267178 伟晶岩 207 43 1720 45.6
267179 伟晶岩 254 107 1910 24.6
267180 伟晶岩 75.1 138 590 24.8
267181 伟晶岩 109 62 1440 7.8
267182 伟晶岩 113 61 1500 8.3
267183 伟晶岩 184 65 1450 22.8
267184 伟晶岩 228 99 1820 92.8
267185 伟晶岩 124 45 1260 15
267186 伟晶岩 37.8 99 334 22.2
267188 伟晶岩 114 50 1230 10
267189 伟晶岩 136 48 1470 9.9
267190 伟晶岩 74.9 212 700 52.8
267191 伟晶岩 30.8 94 291 27.6
267192 伟晶岩 59.1 73 388 36.6
267193 伟晶岩 116 85 1020 20.4
267194 伟晶岩 16.2 79 103 22.6
267198 伟晶岩 9.7 103 285 23.7
267199 伟晶岩 102 539 1580 213
267200 伟晶岩 25.7 184 421 470
267388 伟晶岩 125 72 464 34.1
267389 伟晶岩 124 165 863 41.7
267390 伟晶岩 6.9 36 46 35.6
267391 伟晶岩 11.1 37 35 36.6
267393 伟晶岩 8 30 42 37.4
267394 伟晶岩 49.6 36 410 25.4
267395 伟晶岩 18 203 84 33.1
267396 伟晶岩 27.2 76 114 31.1
267397 伟晶岩 14.7 249 68 20.2
267398 伟晶岩 10.8 235 57 20.6
267400 伟晶岩 346 23 1620 7.2
267428 伟晶岩 237 28 2090 11.9
726881 伟晶岩 13.7 -10 602 29.3

Table 2. Results and highlights from the Bus Lithium Property.

表 2。 巴士锂业的结果和亮点。

Sample # Lithology Cs (ppm) Li (ppm) Rb (ppm) Ta (ppm)
710502 Pegmatite 186 5 1450 82.1
710543 Pegmatite 31.2 121 233 27.4
710544 Pegmatite 28.4 11 232 63.9
710588 Pegmatite 105 155 1690 57.1
710894 Amphibolite 3.8 182 8 0.3
710895 Pegmatite 66 85 1640 11.8
710896 Pegmatite 45.6 93 1430 4.1
710899 Pegmatite 69.8 70 1990 11.5
711000 Pegmatite 42.3 5 1030 14.8
示例 # 岩性学 Cs (ppm) 李 (ppm) Rb (ppm) Ta (ppm)
710502 伟晶岩 186 5 1450 82.1
710543 伟晶岩 31.2 121 233 27.4
710544 伟晶岩 28.4 11 232 63.9
710588 伟晶岩 105 155 1690 57.1
710894 角闪石 3.8 182 8 0.3
710895 伟晶岩 66 85 1640 11.8
710896 伟晶岩 45.6 93 1430 4.1
710899 伟晶岩 69.8 70 1990 11.5
711000 伟晶岩 42.3 5 1030 14.8

Figure 6. Field photos from the 2023 surface exploration campaign at Lithium One properties in the James Bay region of Quebec.

图 6。 2023年魁北克詹姆斯湾地区Lithium One物业的地表勘探活动的实地照片。

The technical content of this news release has been reviewed and approved by Carl Ginn, P.Geo., a Qualified Person pursuant to National Instrument 43-101.

本新闻稿的技术内容已由美国国家仪器43-101规定的合格人员卡尔·金恩(P.Geo.)的审查和批准。

About Lithium One

关于一号锂电池

Lithium One Metals is a Canadian exploration company specializing in the acquisition and development of high-potential lithium properties in Ontario and Québec. Our team of experienced geologists and prospectors are at the forefront of the search for the next generation of lithium deposits.

Lithium One Metals是一家加拿大勘探公司,专门收购和开发安大略省和魁北克省的高潜力锂资产。我们由经验丰富的地质学家和探矿者组成的团队处于寻找下一代锂矿床的最前沿。

On behalf of Lithium One Metals Inc.
Dale Ginn, President and Chief Executive Officer

代表 Lithium One Metals Inc.
戴尔·吉恩,总裁兼首席执行官

For more information, please visit the Company's website at or contact:
Dale Ginn
Tel: +1-604-678-5308
Email: info@lithiumonemetals.com

欲了解更多信息,请访问公司网站或联系:
戴尔·吉恩
电话:+1-604-678-5308
电子邮件:info@lithiumonemetals.com

Neither the TSX Venture Exchange 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.

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。

WARNING: The Company relies upon litigation protection for "forward-looking" statements. The information in this release may contain forward-looking information under applicable securities laws. This forward-looking information is subject to known and unknown risks, uncertainties and other factors that may cause actual results to differ materially from those implied by the forward-looking information. Factors that may cause actual results to vary materially include, but are not limited to, inaccurate assumptions concerning the exploration for and development of mineral deposits, currency fluctuations, unanticipated operational or technical difficulties, changes in laws or regulations, failure to obtain regulatory, exchange or shareholder approval, the risks of obtaining necessary licenses and permits, changes in general economic conditions or conditions in the financial markets and the inability to raise additional financing. Readers are cautioned not to place undue reliance on this forward-looking information. The Company does not assume the obligation to revise or update this forward-looking information after the date of this release or to revise such information to reflect the occurrence of future unanticipated events, except as may be required under applicable securities laws.

警告:公司依靠诉讼保护来提供 “前瞻性” 陈述。根据适用的证券法,本新闻稿中的信息可能包含前瞻性信息。这些前瞻性信息受已知和未知的风险、不确定性和其他因素的影响,这些因素可能导致实际结果与前瞻性信息所暗示的结果存在重大差异。可能导致实际结果出现重大差异的因素包括但不限于有关矿藏勘探和开发的不准确假设、货币波动、意想不到的运营或技术困难、法律或法规的变化、未能获得监管、交易所或股东的批准、获得必要执照和许可证的风险、总体经济条件或金融市场条件的变化以及无法筹集额外资金。提醒读者不要过分依赖这些前瞻性信息。除非适用的证券法另有要求,否则公司没有义务在本新闻稿发布之日之后修改或更新这些前瞻性信息,也没有义务修改此类信息以反映未来意想不到的事件的发生。

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要查看本新闻稿的源版本,请访问

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