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Québec Nickel Corp. Intersects 0.44% Ni, 0.51% Cu and 0.69 G/t Pt-Pd-Au Over 18.50 Metres at Its Ducros Project, Abitibi Québec

Québec Nickel Corp. Intersects 0.44% Ni, 0.51% Cu and 0.69 G/t Pt-Pd-Au Over 18.50 Metres at Its Ducros Project, Abitibi Québec

魁北克镍公司在魁北克Abitibi Ducros项目18.50米内交汇0.44%镍、0.51%铜和0.69G/t铂-钯-金
newsfile ·  2022/05/16 20:39

Continuity drilling of the Fortin Sill Ni-Cu-PGE-Au zone initiated

Fortin Sill Ni-Cu-PGE-Au带开始连续钻井

Vancouver, British Columbia--(Newsfile Corp. - May 16, 2022) - Québec Nickel Corp. (CSE: QNI) (FSE: 7lB) (OTCQB: QNICF) (or the "Company") is pleased to report nickel-copper-PGE-gold drilling assay results from its Ducros Property, 80 kilometres northeast of Val-d'Or, Québec. Drill hole QDG-22-09, which was collared at the Fortin Sill target in the eastern part of the Ducros property, was completed to validate the results returned from the 2008 Golden Valley Mines Ltd. hole GCF-08-07. Hole QDG-22-09 returned a 31 metres-wide intercept averaging 0.37% Ni, 0.40% Cu and 0.55 g/t Pt-Pd-Au, from 10.00 to 41.00 metres hole depth. Included within this 31-metre intercept, are higher grade sub-intervals including 0.44% Ni, 0.51% Cu and 0.69 g/t Pt-Pd-Au over 18.50 and 0.55% Ni, 0.86% Cu and 0.86 g/t Pt-Pd-Au over 5.0 metres.

温哥华,不列颠哥伦比亚省-(Newsfile Corp.-2022年5月16日)-魁北克镍业公司 (CSE:QNI) (FSE:7磅(OTCQB:QNICF)(或“公司“)很高兴地报告其位于魁北克省Val-d‘Or东北80公里处的Ducros矿的镍-铜-PGE-金钻探测试结果。在Ducros矿东部Fortin Sill目标处钻探的QDG-22-09孔已经完成,以验证2008 Golden Valley Mines Ltd.孔GCF-08-07返回的结果。QDG-22-09孔返回了31米宽的截距,平均含0.37%镍、0.40%铜和0.55g/t铂-钯-金,井深10.00~41.00米。在这个31米长的截距内,包括更高等级的亚层段,包括0.44%镍、0.51%铜和0.69g/t铂-钯-金超过18.500.55%镍、0.86%铜和0.86g/t铂-钯-金,超过5.0米.

Highlights:

重点:

  • The near-surface 18.50 metres-long sub-interval, which returned 0.44% Ni, 0.51% Cu and 0.69 g/t Pt-Pd-Au, improves upon the overall grade intersected in the lone historical hole completed at the Fortin Sill target in 2008.
  • A 0.50 metre sample of semi-massive to net texture sulphides contains 1.31% Ni, 0.38% Cu and 2.12 g/t Pt-Pd-Au.
  • The VTEMTM electromagnetic-magnetic anomaly interpreted to lie beneath the Fortin Sill showing has yet to be drilled.
  • 近地表18.50米长的亚层段产出0.44%镍、0.51%铜和0.69g/t铂-钯-金,比2008年在Fortin Sill目标区完成的唯一历史井的整体品位有所改善。
  • 0.50m半块状-网状结构硫化物样品中镍含量为1.31%,铜含量为0.38%,铂-钯-金含量为2.12g/t。
  • VTEM机TM被解释为位于Fortin Sill显示下方的电磁异常尚未被钻探。

Gary DeSchutter, Québec Nickel's Vice President of Exploration, remarks, "I am very fortunate to have worked at several high-quality nickel projects during my career, including at a producing PGE mine, and I can honestly say receiving assay results like these from the Fortin Sill target is very exciting. I'm really looking forward to seeing what else the Fortin Sill target, as well as the rest of this great project, delivers in the coming weeks and months."

魁北克镍业勘探副总裁Gary DeSchutter表示:“在我的职业生涯中,我非常幸运地在几个高质量的镍项目中工作过,包括在一个生产PGE的矿山,我可以诚实地说,从Fortin Sill靶标收到这样的分析结果非常令人兴奋。我真的很期待看到Fortin Sill靶标以及这个伟大项目的其余部分在未来几周和几个月里能带来什么。”

Results from hole QDG-22-09 confirm and improve upon those from the 2008 Golden Valley drill hole which returned 0.38% Ni, 0.44% Cu and 0.65 g/t Pt-Pd-Au over a core interval of 20.7 metres (Québec Assessment report GM65886). The 31-metre-long mineralized intersection from QDG-22-09 represents a greater than 45% increase in intercept length compared to the 2008 Golden Valley hole. In addition, the Ni-Cu-PGE-Au grades within 18.50-metre-long sub-interval in QDG-22-09 are almost 20% higher than those from the 2008 hole. From the current drill hole, a 0.50-metre-long sample collected at 15.50-16.00 metres, which includes pyrrhotite-dominated semi-massive and next texture sulphides, returns 1.31% Ni, 0.38% Cu and 2.12 g/t Pt-Pd-Au (sample E947199, Figure 2). Of note, the 2008 hole did not encounter any semi-massive to net texture sulphides, or the corresponding higher-grade results, as is the case for QDG-22-09.

QDG-22-09孔的结果证实并优于2008年金谷钻孔的结果,该孔在20.7米的岩心间隔内获得0.38%的镍、0.44%的铜和0.65g/t的铂-钯-金(魁北克评估报告GM65886)。QDG-22-09的矿化交汇处长31米,与2008年的金谷洞相比,截距长度增加了45%以上。此外,QDG-22-09中18.50米亚段内的Ni-Cu-PGE-Au品位比2008年提高了近20%。从目前的钻孔中,在15.50-16.00米处采集了一个0.50米长的样品,其中包括以磁黄铁矿为主的半块状硫化物和次要结构的硫化物,其镍含量为1.31%,铜含量为0.38%,铂-钯-金含量为2.12克/吨(样品E947199,图2)。值得注意的是,2008年的洞没有遇到任何半块状到净结构的硫化物,也没有遇到相应的更高等级的结果,就像QDG-22-09的情况一样。

The initial geological interpretation of the Fortin Sill showing is that of a Ni-Cu-Pt-Pd-Au-mineralized differentiated mafic-ultramafic intrusion. This interpretation is supported by observations that the contacts between the different mafic and ultramafic rock units are gradational in nature, as well as the occurrence of brecciated contacts between the mineralized intrusion and host mafic volcanic +/- metasedimentary country rocks. Summary assays results are provided below in Table 1 and photographs of drill core from QDG-22-09 are presented in Figures 1 and 2.

Fortin Sill显示的初步地质解释是一种镍-铜-铂-钯-金矿化分异镁铁质-超镁铁质侵入体。不同的镁铁质和超镁铁质岩石单元之间的接触在性质上是渐变的,以及矿化侵入体与寄主镁铁质火山/变质围岩之间存在角砾状接触,这支持了这一解释。下面的表1提供了分析结果摘要,图1和图2提供了QDG-22-09钻芯的照片。

Sulphide mineralization throughout the 31-metre-long core intersection, which is interpreted to be of primary magmatic in origin, consists of sub-metre to multi-metre-wide zones of interstitial, finely disseminated to patchy magmatic sulphides with subordinate intervals of semi-massive to net-texture sulphides (pyrrhotite + chalcopyrite) intercalated with multi-metre-long intervals containing coarse to very coarse blebby pyrrhotite + chalcopyrite. Host rocks to the sulphide mineralization include mafic and ultramafic intrusive units including gabbro, olivine-bearing gabbro and pyroxenite, with the pyroxenite units having undergone significant greenschist metamorphism-related alteration, essentially turning the rock into a chlorite schist. Further down the hole beyond the Ni-Cu-PGE-mineralized intrusion, the remainder of the 225-metre-long drill hole cored through a mixed sequence of intercalated sheared mafic volcanic and metasedimentary rocks before terminating in a >23-metre-long interval of strongly sheared and quartz-carbonate-veined ultramafic unit that contains trace to locally 1% finely disseminated pyrite + pyrrhotite. The entire length of the hole has been sampled; however, assay results have only been received for the top 79 metres of the hole.

整个31米长的岩心交汇处的硫化物矿化被解释为原生岩浆成因,由宽小于米到数米宽的间隙带组成,细分散到片状岩浆硫化物,从属区间为半块状到网状结构的硫化物(磁黄铁矿+黄铜矿),夹层为数米长的含粗至极粗的气泡状磁黄铁矿+黄铜矿。硫化物矿化的容矿岩石包括镁铁质和超镁铁质侵入岩单元,包括辉长岩、橄榄辉长岩和辉石岩,辉石岩单元经历了与绿片岩变质作用有关的重大蚀变,基本上将岩石转变为绿泥石片岩。在Ni-Cu-PGE矿化侵入体以外的洞中,225米长的钻孔的其余部分穿过一系列夹层剪切的镁铁质火山岩和变质沉积岩,最后终止于一段>23米长的强烈剪切和石英碳酸盐脉状的超镁铁质单元,其中含有微量到局部1%的细小浸染的黄铁矿+磁黄铁矿。已经对整个洞的长度进行了采样;然而,只收到了洞顶部79米的化验结果。

Hole QDG-22-09 was collared several metres to the southwest of the stripped bedrock exposure of the Fortin Sill showing, drilled at a 45° azimuth and at a -45° dip. The drill collar for the original Golden Valley drill hole completed in 2008, GCF-08-07, has not been located since the casing was not left in the BQ diameter hole, but it assumed QDG-22-09 is located within 25 metres to the southwest of the historical hole based on the GPS coordinates provided in the Golden Valley drill log (Québec Assessment report GM65886). The Golden Valley assessment report indicates GCF-08-07 was drilled at a 45° azimuth and at a -45° dip, so it is therefore assumed the trace of QDG-22-09 undercuts the historical hole by +/- 25 metres.

QDG-22-09孔是在Fortin Sill露出的剥离基岩暴露的西南方向几米处钻探的,钻探方位为45°,倾角为-45°。据魁北克评估报告(GM65886)所述,2008年完成的原黄金谷地钻孔GCF-08-07的钻杆一直未找到,因为井筒没有留在BQ直径孔中,但根据金谷钻探日志中提供的全球定位系统坐标,它假定QDG-22-09位于历史孔西南25米范围内。金谷评估报告指出,GCF-08-07是在45°方位和-45°倾角钻进的,因此可以假定QDG-22-09的轨迹比历史上的洞深+/-25米。


Table 1. Summary of assay results from hole QDG-22-091,2,3


表1.QDG-22-09孔化验结果总结1,2,3

1Reported assay intervals are sample length weighted.
2The true width of the mineralized intersection is not known due to insufficient information.
33E = Pt+Pd+Au

1报告的分析间隔是按样本长度加权的。
2由于信息不足,矿化交叉口的真实宽度尚不清楚。
33E=铂+钯+金

Additional holes are being drilled from the same set-up as QDG-22-09 to establish the continuity of the Ni-Cu-PGE-Au mineralization both on and off drill section and assay results will be reported from these holes once received. A drill hole to test the VTEMTM electromagnetic-magnetic anomaly, interpreted to lie directly beneath the Fortin Sill showing, will also be completed in the coming weeks (please refer to the April 27, 2022, News Release for details regarding this specific geophysical drill target). Additionally, Abitibi Geophysics, who's head office is in Val-d'Or, is currently at the Ducros project completing time domain borehole electromagnetic surveys within several of the key drill holes completed during the 2022 work program to date. This borehole EM work is being done to follow-up on the semi-massive sulphide intersection in QDG-22-09 as well as to guide future drilling efforts towards finding additional accumulations of electrically conductive Ni-Cu-PGE-Au-rich sulphides in the Fortin Sill target area.

正在从与QDG-22-09相同的设置中钻取更多的孔,以确定开钻和停钻段的Ni-Cu-PGE-Au矿化的连续性,一旦收到这些孔的分析结果,将立即报告。一种测试垂直瞬变电磁波的钻孔TM电磁异常,解释为位于Fortin Sill显示的正下方,也将在未来几周内完成(有关这一特定地球物理钻探目标的详细信息,请参阅2022年4月27日的新闻稿)。此外,总部设在Val-d‘Or的Abitibi地球物理公司目前正在Ducros项目中完成2022年工作计划迄今完成的几个关键钻孔内的时域钻孔电磁测量。这项钻孔电磁工作是为了跟踪QDG-22-09的半块状硫化物交汇处,并指导未来的钻探工作,以便在Fortin Sill目标区发现更多的导电镍-铜-铂族-金硫化物聚集层。

Additional drill holes are being designed to follow-up on these results and will be submitted for permitting in the coming days.

正在设计更多的钻孔来跟进这些结果,并将在未来几天提交许可。

Core Processing & QAQC
Québec Nickel has implemented a quality assurance and quality control ("QAQC") program for its drilling program, to ensure best practice for logging, sampling, and analysis of its drill core, and includes the regular insertion of geochemical blanks and two different Ni-Cu-PGE certified reference material standards (CRM's) into the sample stream.

核心处理和QAQC
魁北克镍业为其钻探计划实施了质量保证和质量控制(“QAQC”)计划,以确保其钻芯的录井、采样和分析的最佳实践,并包括定期在样品流中插入化探空白和两种不同的经Ni-Cu-PGE认证的标准物质(CRM)。

Drill core is collected by Ducros project personnel from the drill daily and transported to QNI's core logging facility in Val d'Or in secured core boxes. Logging is completed on a laptop and data are captured using fit-for-purpose computer software. In addition to recording geological, structural, mineralogical, and alteration data, QNI personnel also collect Rock Quality Designation (RQD) data for all core runs, as well as Specific Gravity, Magnetic Susceptibility and Conductivity measurements at regular intervals. All drill core is photographed both dry and wet prior to sampling.

钻芯由Ducros项目人员每天从钻探中收集,并装在安全的岩芯盒中运往QNI位于Val d‘Or的岩心测井设施。记录在笔记本电脑上完成,并使用适合用途的计算机软件捕获数据。除了记录地质、构造、矿物学和蚀变数据外,QNI人员还定期收集所有岩心的岩石质量指定(RQD)数据,以及比重、磁化率和电导率测量数据。所有钻芯在取样前都要拍摄干的和湿的照片。

Core sample lengths typically vary between 30 centimetres to 1.50 metres, dependant on geological and mineralization contacts. Core destined for geochemical analyses is sawed in half by a diamond blade saw with clean uncirculated water, and one half of the core is returned to the core box for archiving while the other half is placed in labeled and sealed sample bags and sent to the laboratory for analyses. All samples are transported from QNI's logging facility to AGAT Laboratories' sample preparation facility in Val-d'Or in secured and numbered rice bags by project personnel.

岩心样品的长度通常在30厘米至1.50米之间,取决于地质和矿化接触。用于地球化学分析的岩芯用金刚石锯片锯成两半,用干净的未循环水切割,一半返回岩芯盒存档,另一半放在有标签和密封的样品袋中,送往实验室进行分析。项目人员将所有样品从QNI的测井设施运送到位于Val-d‘Or的AGAT实验室的样品制备设施,装在安全的带编号的大米袋中。

AGAT Laboratories is accredited to the ISO/IEC 17025:2017 and ISO 9001:2015 standards. Analysis for precious metals (gold, platinum, and palladium) is completed by Fire Assay with an ICP-OES finish while analyses for nickel, copper, and 41 other elements are performed using AGAT's 4 Acid Digest - Metals Package, with an ICP-OES finish.

雅加特实验室通过了国际标准化组织/国际电工委员会17025:2017年和国际标准化组织9001:2015年标准认证。贵金属(金、铂和钯)的分析通过火焰分析和电感耦合等离子体发射光谱完成,而镍、铜和其他41种元素的分析则使用AGAT的4 ACID Digest-Metals套装和电感耦合等离子体发射光谱完成。

QUALIFIED PERSON
Gary DeSchutter, M.Sc., P.Geo., Vice-President of Exploration for Québec Nickel Corp., and a Qualified Person ("QP") as defined under National Instrument 43-101 ("NI 43-101"), has reviewed, and approved the scientific and technical content of this press release.

有资格的人
魁北克镍业公司勘探副总裁Gary DeSchutter,M.Sc,P.Geo,National Instrument 43-101(“NI 43-101”)定义的合格人士(“QP”)已审核并批准了本新闻稿中的科学技术内容。

ABOUT QUEBEC NICKEL CORP.
Québec Nickel Corp. is a mineral exploration company focused on acquiring, exploring, and developing nickel projects in Québec, Canada. The Company has a 100% interest in the Ducros Property, consisting of 280 contiguous mining claims covering 15,147 hectares within the eastern portion of the Abitibi Greenstone Belt in Québec, Canada. Additional information on Québec Nickel Corp. is available at .

关于魁北克镍公司。
魁北克镍公司是一家专注于收购、勘探和开发加拿大魁北克镍项目的矿产勘探公司。本公司拥有Ducros矿产的100%权益,包括加拿大魁北克省Abitibi Greenstone带东部的280个毗连矿权,占地15,147公顷。欲了解更多有关魁北克镍业公司的信息,请访问。

The CSE has neither approved nor disapproved the contents of this news release. Neither the CSE nor its Market Regulator (as that term is defined in the policies of the CSE) accepts responsibility for the adequacy or accuracy of this release.

CSE既没有批准也没有不批准本新闻稿的内容。CSE及其市场监管机构(该术语在CSE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。

On behalf of the Board of Directors

我谨代表董事会

David Patterson
Chief Executive Officer and Director

大卫·帕特森
董事首席执行官兼首席执行官

1 (855) 764-2535 (QNICKEL)
info@quebecnickel.com

1(855)764-2535(QNICKEL)
邮箱:info@quebecickel.com

CAUTIONARY AND FORWARD-LOOKING STATEMENTS

警告性和前瞻性陈述

This news release includes certain statements that may be deemed "forward-looking statements". All statements in this news release, other than statements of historical facts that address events or developments that the Company expects to occur, are forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words "expects," "plans," "anticipates," "believes," "intends," "estimates," "projects," "potential" and similar expressions, or that events or conditions "will," "would," "may," "could" or "should" occur. Although the Company believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance, and actual results may differ materially from those in the forward-looking statements. Factors that could cause the results to differ materially from those in forward-looking statements include market prices, continued availability of capital and financing, and general economic, market, or business conditions. Investors are cautioned that such statements are not guarantees of future performance and that actual results or developments may differ materially from those projected in the forward-looking statements. Forward-looking statements are based on the beliefs, estimates, and opinions of the Company's management on the date the statements are made. Except as required by applicable securities laws, the Company undertakes no obligation to update these forward-looking statements if management's beliefs, estimates, opinions, or other factors should change.

本新闻稿包括可被视为“前瞻性陈述”的某些陈述。除涉及公司预期发生的事件或发展的历史事实陈述外,本新闻稿中的所有陈述均为前瞻性陈述。前瞻性陈述是指不是历史事实的陈述,通常但并非总是由“预期”、“计划”、“预期”、“相信”、“打算”、“估计”、“项目”、“潜在”和类似的表述,或事件或条件“将”、“将”、“可能”、“可能”或“应该”发生。尽管公司认为这些前瞻性陈述中表达的预期是基于合理的假设,但这些陈述并不是对未来业绩的保证,实际结果可能与前瞻性陈述中的结果大不相同。可能导致结果与前瞻性陈述中的结果大不相同的因素包括市场价格、资本和融资的持续可获得性以及总体经济、市场或商业状况。请投资者注意,此类陈述并不能保证未来的业绩,实际结果或发展可能与前瞻性陈述中所预测的大不相同。前瞻性陈述是基于公司管理层在陈述发表之日的信念、估计和意见。除非适用的证券法要求,否则如果管理层的信念、估计、意见或其他因素发生变化,公司没有义务更新这些前瞻性陈述。

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要查看本新闻稿的源版本,请访问

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