Renforth exposes 130m of continuous visible nickel and zinc mineralization on surface at Surimeau to date in stripping program
Renforth exposes 130m of continuous visible nickel and zinc mineralization on surface at Surimeau to date in stripping program
TheNewswire - October 14, 2021 - Renforth Resources Inc. (CNSX:RFR.CN) (OTC:RFHRF) (FSE:9RR) ("Renforth" or the "Company") is pleased to update shareholder on the ongoing stripping program on the ~5km long Victoria West target of Renforth's wholly owned 260km2 Surimeau property, located in the Pontiac sediments, contiguous to the Canadian Malartic Mine, near Malartic Quebec.
新闻通讯社-2021年10月14日-Renforth Resources Inc.(CNSX:RFR.氯化萘)(场外交易:RFHRF)(证券交易所:9RR)(“雷福斯”或“公司”)很高兴向股东通报正在进行的关于雷福斯全资拥有的260公里长约5公里的维多利亚西目标的剥离计划的最新情况。2Surimeau地产位于庞蒂亚克沉积物中,毗邻加拿大马拉蒂克矿山,靠近马拉蒂克魁北克。
The program, targeting an area between two of the holes drilled in the 2.2km long drill program earlier this year, is currently paused for a 10-day period to allow local hunters use of the land unimpeded by the stripping operation which has successfully exposed 130m of sulphide bearing bedrock, approximately 40% of the strike expected to be exposed.
该计划的目标是今年早些时候在2.2公里长的钻探计划中钻出的两个孔之间的区域,目前暂停了10天,以允许当地猎人不受剥离作业的阻碍使用土地。剥离作业已成功暴露了130米含硫化物的基岩,约占预计暴露的打击的40%。
Almost all the newly exposed bedrock in the stripped area is ultramafic, hosting low grade nickel and zinc mineralization along the entire strike, with the width of the stripped area averaging 35m in width but reaching up to a maximum of 42m, without exposing the contact of the ultramafic and the sedimentary Pontiac unit. It is anticipated that the north and south crosscuts, once stripped, will expose this contact zone. The mineralized zone, comprised of a central deformational structure bound to the north and the south by ultramafics, is oriented east-west and encompasses, in the western half of the planned stripping area, two small historic trenches which expose the deformation zone and ultramafics. Mineralization has been observed in numerous places within the stripped area visually, confirmed with the use of a handheld XRF. The strongest and most impressive mineralization, at least visually, is along and within the central deformation structure with frequent clots and stringers of chalcopyrite, pyrite, pyrrhotite and occasionally sphalerite and bornite. To date, the first two channels have been cut and sampled and numerous grab samples have been taken. All samples taken before the 10-day break have been delivered to a lab for analysis.
剥离区几乎所有新暴露的基岩都是超镁铁质的,沿整个走向赋存着低品位的镍和锌矿化,剥离区的宽度平均为35m,但最大可达42m,没有暴露超镁铁质与沉积庞蒂亚克单元的接触。预计南北横切一旦被剥离,将暴露这一接触区。矿化带由一个中央变形构造组成,由超镁质岩将南北连接起来,呈东西走向,在规划剥离区的西半部包括两条暴露变形带和超镁岩质的历史小海沟。在剥离区内的许多地方已经目测到矿化,并用手持XRF证实了这一点。最强烈和最令人印象深刻的矿化(至少从视觉上看)是沿着中心变形构造和在中央变形构造内,经常出现黄铜矿、黄铁矿、磁黄铁矿的凝块和条带,偶尔还有闪锌矿和斑铜矿。到目前为止,已经对前两个渠道进行了切割和采样,并采集了大量的抓取样本。在10天假期前采集的所有样本都已被送往实验室进行分析。
Geological Description
地质描述
The deformation zone, oriented approximately east-west and found within the larger ultramafic mass to the north and south and appears on surface with widths that vary from a half-meter to several meters, is often albitized, occasionally with bands of calc-silicate alteration with bright green cr-diopside crystals. Moving north from the deformation zone the rock becomes finer grained and more mafic in composition. The bedrock to the south, also ultramafic in composition, is massive and seems to be much less deformed than the bedrock to the north. There are occasional small-scale faults and shear bands in the bedrock south of the main structure.
变形带大致由东向西,位于南北方向较大的超镁铁质块体内,出现在地表,宽度从半米到几米不等,通常是钠长石,偶尔还会有钙硅酸盐蚀变带和亮绿色的铬辉石晶体。从变形带向北移动,岩石变得更细粒,成分更镁铁质。南边的基岩成分也是超镁铁质的,它很大,看起来比北边的基岩变形小得多。主体构造南侧基岩中偶有小规模断裂和剪切带。
There is a secondary structure that appears to be a splay or deflection of the main deformation zone, possibly caused by a large ultramafic mass forming a tall ridge in the rough center of the stripped area. This is north of the main structure and is a wide deformation zone where the bedrock is frequently blocky with occasional bands of strong shearing and albitization within this zone. These bands are very similar in appearance to what has been observed in the main deformation zone but are not as strongly mineralized. The strike of this wide deformation zone is 100 degrees, but it gradually changes to roughly east west as it meets the main structure towards the eastern end of the current work area.
二次构造似乎是主变形带的张开或偏转,可能是由于在剥离区的粗略中心形成了一条高大的山脊而形成的大型超镁铁质块体所致。这是一个主要构造的北面,是一个宽广的变形带,基岩经常是块状的,在这个带内偶尔会有强烈的剪切和钠长石带。这些带在外观上与在主变形带中观察到的非常相似,但矿化程度不是很高。这一宽阔变形带的走向为100度,但随着它与当前工作区东端的主体构造相遇,它逐渐变成了大致的东西走向。
There is an alteration halo (mainly albite, maybe some carbonate alteration as well) that seems to be only present within the main structure and in the wall rock to the north – the alteration halo appears to be about 3-5m thick at its widest point. The intensity of the albitization decreases to the north, but there are occasional bands of strong shearing and albitization within the wide deformation zone north of the main structure. The strongest and most impressive mineralization, at least visually, is along and within the central deformation structure with frequent clots and stringers of chalcopyrite, pyrite, pyrrhotite and occasionally sphalerite and bornite. Pentlandite has not yet been observed within the main structure, only within the bedrock north of the central deformation structure, within the alteration halo. Alteration in the bedrock south of the main structure is much less intense and mineralization is patchy with rare clots of sulfide-mineralization, mainly pyrrhotite.
有一个蚀变晕(主要是钠长石,可能也有一些碳酸盐蚀变)似乎只存在于主体构造和北面的围岩中-蚀变晕最宽处似乎有3-5m厚。钠长石化强度向北减弱,但在主体构造以北的宽阔变形带内偶有强剪切和钠长石化带。最强烈和最令人印象深刻的矿化,至少在视觉上,是沿着中心变形结构和在中心变形结构内,有频繁的黄铜矿凝块和条带,黄铁矿、磁黄铁矿,偶尔还有闪锌矿和斑铜矿。目前还没有在主体构造内观察到绿柱石,仅在中央变形构造以北的基岩内,蚀变晕内。主体构造以南基岩蚀变强度小得多,矿化呈斑块状,少见硫化物矿化凝块,主要为磁黄铁矿。
There is no graphitic shale exposed in the trenching to date, this is where a significant amount of sphalerite has been identified in drill core. The graphitic shale is observed on surface in other locations on the property but may not be present within the confines of the permitted area.
到目前为止,在海沟中没有发现石墨质页岩,这是在钻芯中发现大量闪锌矿的地方。石墨化页岩可在该物业其他位置的地表上观察到,但可能不在许可区域的范围内。(工业和信息化部电子科学技术情报研究所陈皓)
Once stripping is completed in the east, work will move towards the west end to begin expanding the two historic trenches which we have visited in the past and continue to work west from there. Additionally, the eastern and western north-south oriented crosscuts also need to be stripped where we may expose the contacts of the ultramafics with the sediments or possibly mafic volcanics if present.
一旦东部完成剥离,工作将向西端推进,开始扩建我们过去参观过的两个历史性的战壕,并从那里继续向西工作。此外,东部和西部南北走向的横切也需要剥离,在那里我们可能会暴露超镁质岩与沉积物的接触,或者可能与镁铁质火山岩(如果存在)的接触。
Stripped Area to Date, Looking East
到目前为止剥离的区域,向东看
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The central deformation zone is stained orange (oxidized), to the right is the ultramafics in the south, to the left is the altered ultramafics to the north.
中央变形带呈橙色(氧化),右边是南面的超镁岩带,左边是北面的蚀变超镁岩带。
Main Structure, strongly oxidized and weathered. Looking North
主体结构,强氧化、风化。朝北看
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Zinc Oxidation in Stripped Area after 4 Days of Exposure
暴露4天后剥离区的锌氧化
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Mineralized Fine Sulphide Stringers in Grab Sample
抓取样品中的矿化细硫化物管柱
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The stripping program, along with channel sampling, will resume next week at Surimeau and is anticipated to continue until early November.
剥离计划以及频道采样将于下周在苏里莫恢复,预计将持续到11月初。
Technical disclosure in this press release has been reviewed and approved by Francis R. Newton P.Geo (OGQ#2129), a "qualified person" pursuant to NI 43-101
本新闻稿中的技术披露已由弗朗西斯·R·牛顿P.Geo(OGQ#2129),符合NI 43-101的“合格人员”
For further information please contact:
如需更多信息,请联系:
Renforth Resources Inc.
雷福斯资源公司
Nicole Brewster
妮可·布鲁斯特
President and Chief Executive Officer
总裁兼首席执行官
C:416-818-1393
C:416-818-1393
E: nicole@renforthresources.com
电子邮件:nicole@renforources.com
#269 – 1099 Kingston Road, Pickering ON L1V 1B5
#269-1099金斯顿路,L1V 1B5上的皮克林
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About Renforth
关于雷福斯
Renforth holds the Parbec open pit constrained gold deposit in Malartic Quebec, contiguous to the Canadian Malartic mine, with a 2020 resource estimate of 104,000 indicated ounces of gold at a grade of 1.78 g/t Au and 177,000 inferred ounces of gold at a grade of 1.78 g/t Au. This resource estimate is now considered by Renforth to be out of date due to the results received in a 15,569m drill program which has been recently completed. This program was planned to twin, infill and undercut existing drill holes at Parbec, to support a rebuild of the geological model and a resource estimate restatement. In addition to this Renforth wholly owns the 260 km2 Surimeau District Property with several areas of historically identified polymetallic and gold mineralization. This includes the Victoria West occurrence, Renforth's current focus, interpreted to be a nickel-containing ultramafic unit, juxtaposed with VMS-style copper-zinc mineralization which occurs over ~5km of strike in the western end of the 20km central anomaly at Surimeau. Renforth also holds the Malartic West property, the site of a copper/silver discovery, and Nixon-Bartleman, west of Timmins Ontario, with gold present on surface over a strike length of ~500m. Renforth is well funded, with ~$5 million in cash and securities on hand (*as at 05/14/21), in addition to the gold contained in our gold deposit.
Renforth拥有与加拿大Malartic矿毗邻的魁北克Malartic矿的Parbec露天受限金矿,2020年资源估计为104,000指示盎司黄金,品位为1.78克/吨Au,推断黄金为177,000盎司,品位为1.78 g/t Au。由于最近完成的15569米钻探计划收到的结果,Renforth现在认为这一资源估计已经过时。该项目计划对帕贝克现有的钻孔进行翻转、填塞和挖方,以支持地质模型的重建和资源估算的重述。除此之外,Renforth全资拥有260公里2苏里莫地区拥有几个历史上已确定的多金属矿化和金矿化区域。这包括雷福斯目前的焦点维多利亚西矿体,解释为含镍超镁铁质单元,与VMS式铜锌矿化并列在苏里莫20公里中心异常西端超过5公里的走向上。Renforth还拥有马拉蒂克西部(Malartic West)和尼克松-巴特尔曼(Nixon-Bartleman),马拉蒂克西部是发现铜/银的地点,尼克松-巴特尔曼位于安大略省蒂明斯以西,地表金矿的走向长度超过500米。瑞福斯公司资金雄厚,除了我们的黄金储备外,手头还有大约500万美元的现金和证券(*截至5月14日)。
No securities regulatory authority has approved or disapproved of the contents of this news release.
没有证券监督管理机构批准或不批准本新闻稿的内容。
Forward Looking Statements
前瞻性陈述
This news release contains forward-looking statements and information under applicable securities laws. All statements, other than statements of historical fact, are forward looking. Forward-looking statements are frequently identified by such words as ‘may', ‘will', ‘plan', ‘expect', ‘believe', ‘anticipate', ‘estimate', ‘intend' and similar words referring to future events and results. Such statements and information are based on the current opinions and expectations of management. All forward-looking information is inherently uncertain and subject to a variety of assumptions, risks and uncertainties, including the speculative nature of mineral exploration and development, fluctuating commodity prices, the risks of obtaining necessary approvals, licenses and permits and the availability of financing, as described in more detail in the Company's securities filings available at www.sedar.com. Actual events or results may differ materially from those projected in the forward-looking statements and the reader is cautioned against placing undue reliance thereon. Forward-looking information speaks only as of the date on which it is provided and the Company assumes no obligation to revise or update these forward-looking statements except as required by applicable law.
根据适用的证券法,本新闻稿包含前瞻性陈述和信息。除有关历史事实的陈述外,所有陈述均为前瞻性陈述。前瞻性陈述经常被诸如“可能”、“将”、“计划”、“预期”、“相信”、“预期”、“估计”、“打算”等词汇以及与未来事件和结果有关的类似词汇所标识。这些陈述和信息是基于管理层当前的意见和期望。所有前瞻性信息本质上都是不确定的,受到各种假设、风险和不确定因素的影响,包括矿产勘探和开发的投机性、商品价格的波动、获得必要批准、许可证和许可的风险以及融资的可能性,这些都在该公司提交给www.sedar.com的证券申报文件中有更详细的描述。实际事件或结果可能与前瞻性陈述中预测的大不相同,敬请读者不要过分依赖。向前-前瞻性信息仅在提供之日发表,除非适用法律要求,否则公司不承担修改或更新这些前瞻性陈述的义务。
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