Palladium One Drilling Confirms Multiple Chonolith-Feeder Dyke Structures and Discovers New Ni Mineralization at Tyko Ni - Cu Project
Palladium One Drilling Confirms Multiple Chonolith-Feeder Dyke Structures and Discovers New Ni Mineralization at Tyko Ni - Cu Project
Toronto, Ontario--(Newsfile Corp. - February 1, 2024) - Palladium One Mining Inc. (TSXV: PDM) (OTCQB: NKORF) (FSE: 7N11) (the "Company" or "Palladium One") is pleased to announce initial results from the 2023 drill program on the Tyko I Property, which forms part of the larger Tyko Nickel-Copper Project in Ontario, Canada.
安大略省多倫多--(Newsfile Corp.-2024 年 2 月 1 日)- Palladium One 礦業公司 (TSXV: PDM)(OTCQB: NKORF)(費用:7N11) (那個”公司“或”鈀金一號“)很高興地宣佈2023年Tyko I地產鑽探計劃的初步結果,該地產是加拿大安大略省較大的泰科鎳銅項目的一部分。
Highlights
亮點
New areas of nickel mineralization and new Chonolith / Feeder Dyke structures have been discovered.
In the West Pickle Area, Chonolith / Feeder Dyke structures now extend over more than five kilometers of strike length (Figure 1).
A new nickel zone has been identified with intercepts returning up to 0.4% Ni and 0.2% Cu over 2.7 meters including 1.0% Ni and 0.4% Cu over 0.9 meters in hole TK23-128 in an area with soil anomalies as high as 0.15% Ni, 0.27% Cu and 86 parts per billion ("ppb") Pd + Pt (Figure 2).
Drilling along the eastern margin of the West Pickle Zone targeted bore hole electromagnetic anomalies ("BHEM") returned 1.8% Ni and 1.0% Cu over 1.5 meters in hole TK23-134.
3D modelling of the West Pickle Zone geology following a Magneto Telluric ("MT") survey suggest the zone continues at least 500 meters further northeast, where it intersected magnetic and soil anomalies associated with a newly confirmed ultramafic Chonolith / Feeder Dyke structure (Figure 3).
In Q4 2023, 3,023 meters were drilled in 22 diamond drill holes on the Tyko projects, 12 holes drilled on the Tyko I property are detailed in this release.
已經發現了新的鎳礦化區域和新的 Chonolith/Feeder Dyke 結構。
在西皮克爾地區,Chonolith/Feeder Dyke 結構現在的攻擊長度已超過五千米(圖 1)。
已經發現了一個新的鎳區,其截距在2.7米處返回高達0.4%的鎳和0.2%的銅,包括 0.9 米以上,鎳含量爲 1.0%,銅含量爲 0.4% 在土壤異常高達 0.15% 鎳、0.27% 銅和十億分之86(“ppb”)鈀+鉑的土壤異常區域的 TK23-128 孔中(圖 2)。
在西皮克爾區東緣鑽探的目標鑽孔電磁異常(“BHEM”)再次出現 1.5 米以上,鎳含量爲 1.8%,銅含量爲 1.0% 在洞裏 TK23-134。
在大地磁學(“MT”)調查之後對西泡菜區地質進行了三維建模,結果表明,該區域向東北延伸至少 500 米,在那裏它與新確認的超鎂鐵質Chonolith/Feeder Dyke結構相關的磁和土壤異常相交(圖 3)。
2023年第四季度,泰科項目的22個鑽石鑽孔鑽探了3,023米,在本新聞稿中詳細介紹了在Tyko I地產上鑽探的12個孔。
"Tyko's new nickel district geologic model continues to be confirmed with the 2023 drilling program. The discovery of an additional zone of high-grade nickel mineralization (hole TK23-128) at shallow depth is highly encouraging. Notably the MT anomaly extending east of the West Pickle Zone remains to be tested along with other priority targets, while additional exploration permits will be required in advance of drilling," stated Derrick Weyrauch, President and CEO.
“Tyko的新鎳礦區地質模型繼續得到2023年鑽探計劃的證實。在較淺的深度發現了另外一個高品位鎳礦化區域(TK23-128 孔),這非常令人鼓舞。值得注意的是,延伸到西皮克爾區以東的MT異常以及其他優先目標仍有待測試,而在鑽探之前還需要額外的勘探許可。” 總裁兼首席執行官德里克·韋勞赫表示。
The 2023 drill program comprised 22 holes totalling 3,023 meters on both the Tyko I and Tyko II properties. The program included 12 holes targeting the West Pickle area of Tyko I which form this release. Drilling in the West Pickle area was designed to be shallow and to test for near surface mineralization proximal to soil anomalies previously reported. Deeper drill testing of the Magneto Telluric ("MT) geophysical anomaly (see news release October 30, 2023) that could connect West Pickle to the RJ Zone (four to five kilometers to the east), and the Gionet Zone on Tyko II (see news release November 21, 2023) will require additional exploration permits.
2023 年的鑽探計劃包括在 Tyko I 和 Tyko II 地產上的 22 個鑽孔,總長 3,023 米。該項目包括針對Tyko I西皮克爾區域的12個洞,這些洞構成了本版本。西皮克爾地區的鑽探設計爲淺層鑽探,用於測試先前報告的土壤異常附近的近地表礦化。對可能將西皮克爾與RJ區域(向東四到五千米)以及Tyko II的吉奧內特區(見2023年11月21日新聞稿)連接起來的大地電磁(“MT”)地球物理異常(見2023年11月21日新聞稿)的更深鑽探測試將需要額外的勘探許可。
The result of the drill program successfully intersected significant ultramafic rocks confirming the Chonolith / Feeder Dyke model. Two new large areas of ultramafic rocks were outlined confirming previous soil and geophysical anomalies. However, the amount of sulphide Ni-Cu mineralization intersected in drilling is less than suggested by nearby soil anomalies, indicating that additional mineralization exist and additional drilling is warranted. Future exploration plans include trenching, mapping and channel sampling to better understand the controls on this new mineralization followed by drill testing.
鑽探計劃的結果成功地與大量的超鎂鐵質岩石相交,證實了Chonolith/Feeder Dyke模型。概述了兩塊新的大面積超鎂鐵質岩石,證實了先前的土壤和地球物理異常。但是,鑽探中相交的硫化物鎳銅礦化量低於附近土壤異常所暗示的量,這表明存在額外的礦化,需要進行更多鑽探。未來的勘探計劃包括挖溝、測繪和河道採樣,以更好地了解對這種新礦化的控制,然後進行鑽探測試。
The most significant result of the program was a new area of high-grade Ni-Cu mineralization intersected 1 kilometer northwest of the West Pickle Zone, in an area with significant Ni-Cu-PGE soil anomalies having up to 0.15% Ni, 0.27% Cu and 69 ppb Pd and 17 ppb Pt in soils (Figure 1 and 2). These anomalies were offset from the magnetic high suggesting more extensive non-magnetic ultramafic rocks in the area. Hole TK23-128 intersected sheared Ni-Cu sulphide mineralization in altered pyroxenitic rocks returning 0.4% Ni and 0.2% Cu over 2.7 meters including 1.0% Ni and 0.4% Cu over 0.9 meters (Figure 1 and 2).
該項目最顯著的成果是,在西泡菜區西北1公里處有一個新的高品位鎳銅礦化區域,該地區存在嚴重的鎳銅鉑土壤異常,土壤中鎳含量高達0.15%,銅含量高達69ppb,鈀含量高達17ppb(圖1和2)。這些異常被磁高點所抵消,這表明該地區存在更廣泛的非磁性超鎂鐵質岩石。TK23-128 孔在變質輝石巖中與剪切後的鎳銅硫化物礦化層相交,在 2.7 米處返回 0.4% 的鎳和 0.2% 的銅,包括 0.9 米以上,鎳含量爲 1.0%,銅含量爲 0.4% (圖 1 和 2)。
Two holes tested Maxwell plates modelled form Borehole Electromagnetic ("BHEM") surveys on the West Pickle Zone (Figure 1 and 2). Hole TK22-133 did not intersect any mineralization or ultramafic rocks, the source of the Maxwell plate remains unexplained. Hole TK23-134 intersected the modelled Maxwell plate returning 1.8% Ni and 1.0% Cu over 1.5 meters. The West Pickle Zone horizon remains open to both the east and west.
兩個孔測試了以西泡菜區鑽孔電磁(“BHEM”)調查爲模型的麥克斯韋板塊(圖 1 和 2)。TK22-133 孔沒有與任何礦化岩石或超鎂鐵質岩石相交,麥克斯韋板塊的來源仍無法解釋。TK23-134 孔與仿真的 Maxwell 板相交 1.5 米以上,鎳含量爲 1.8%,銅含量爲 1.0%。西泡菜區的地平線仍然向東和向西開放。
About Tyko Nickel - Copper - Cobalt Project
The Tyko Nickel - Copper - Cobalt Project, is located approximately 65 kilometers northeast of Marathon Ontario, Canada. Tyko is an early stage, high sulphide tenor, nickel - copper (2:1 ratio) project and with multiple mineralized zones spanning over a 20-kilometer strike length and demonstrating the potential for a new greenfield nickel district.
關於 Tyko Nickel-Copper-Cobalt 項目
泰科鎳業——銅——鈷項目位於加拿大安大略省馬拉松市東北約65公里處。Tyko是一個處於早期階段、高硫化物含量、鎳-銅(比例爲 2:1)的項目,其多個礦化區跨越20千米的走向長度,這表明了新建鎳礦區的潛力。
Qualified Person
The technical information in this release has been reviewed and verified by Neil Pettigrew, M.Sc., P. Geo., Vice President of Exploration and a director of the Company and the Qualified Person as defined by National Instrument 43-101.
合格人員
本新聞稿中的技術信息已由理學碩士、P. Geo.、勘探副總裁、公司董事兼National Instrument 43-101定義的合格人員Neil Pettigrew進行了審查和驗證。
About Palladium One
Palladium One Mining Inc. (TSXV: PDM) is focused on discovering environmentally and socially conscious Critical Green Transportation Metals. A Canadian mineral exploration and development company, Palladium One is targeting district scale, nickel - copper sulphide and platinum-group-element (PGE) deposits in Canada and Finland. The Läntinen Koillismaa (LK) Project in north-central Finland, is a PGE-copper-nickel project that has existing NI43-101 Mineral Resources, while both the Tyko and Canalask high-grade nickel-copper projects are located in Ontario and the Yukon, Canada, respectively. Follow Palladium One on LinkedIn, Twitter, and at .
關於 Palladium One
Palladium One Mining Inc.(多倫多證券交易所股票代碼:PDM)專注於發現具有環境和社會意識 關鍵的綠色運輸金屬。加拿大礦產勘探和開發公司Palladium One的目標是加拿大和芬蘭的地區規模、硫化鎳銅和鉑族元素(PGE)礦牀。位於芬蘭中北部的Lantinen Koillismaa(LK)項目是一個 PGE-Copper-Nickel 項目,擁有 NI43-101 礦產資源,而 Tyko 和 Canalask 的高品位鎳銅項目分別位於加拿大安大略省和育空地區。在 LinkedIum、Twitter 等上關注 Palladium One
ON BEHALF OF THE BOARD
"Derrick Weyrauch"
President & CEO, Director
代表董事會
“Derrick Weyrauch”
總裁兼首席執行官、董事
For further information contact:
Derrick Weyrauch, President & CEO
Email: info@palladiumoneinc.com
欲了解更多信息,請聯繫:
德里克·韋勞赫,總裁兼首席執行官
電子郵件: info@palladiumoneinc.com
Neither the TSX Venture Exchange nor its Market Regulator (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
多倫多證券交易所風險交易所及其市場監管機構(該術語在多倫多證券交易所風險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。
This press release is not an offer or a solicitation of an offer of securities for sale in the United States of America. The common shares of Palladium One Mining Inc. have not been and will not be registered under the U.S. Securities Act of 1933, as amended, and may not be offered or sold in the United States absent registration or an applicable exemption from registration.
本新聞稿不是在美利堅合衆國出售證券的要約或邀請。根據經修訂的1933年《美國證券法》,Palladium One Minining Inc.的普通股過去和將來都不會註冊,未經註冊或適用的註冊豁免,不得在美國發行或出售。
Information set forth in this press release may contain forward-looking statements. Forward-looking statements are statements that relate to future, not past events. In this context, forward-looking statements often address a company's expected future business and financial performance, and often contain words such as "anticipate", "believe", "plan", "estimate", "expect", and "intend", statements that an action or event "may", "might", "could", "should", or "will" be taken or occur, or other similar expressions. By their nature, forward-looking statements involve known and unknown risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events, to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements. Such factors include, among others, risks associated with project development; the need for additional financing; operational risks associated with mining and mineral processing; fluctuations in mineral and commodity prices; title matters; environmental liability claims and insurance; reliance on key personnel; the absence of dividends; competition; dilution; the volatility of our common share price and volume; and the impact of governmental entities. Forward-looking statements are made based on management's beliefs, estimates and opinions on the date that statements are made and the Company undertakes no obligation to update forward-looking statements if these beliefs, estimates and opinions or other circumstances should change. Investors are cautioned against attributing undue certainty to forward-looking statements
本新聞稿中提供的信息可能包含前瞻性陳述。前瞻性陳述是與未來事件相關的陳述,而不是與過去的事件相關的陳述。在這種情況下,前瞻性陳述通常涉及公司的預期未來業務和財務業績,通常包含 “預期”、“相信”、“計劃”、“估計”、“預期” 和 “打算” 等詞語,關於某項行動或事件 “可能”、“可能”、“應該” 或 “將” 採取或發生的陳述,或其他類似的表述。就其性質而言,前瞻性陳述涉及已知和未知的風險、不確定性和其他因素,這些因素可能導致我們的實際業績、業績或成就或其他未來事件與此類前瞻性陳述所表達或暗示的任何未來業績、業績或成就存在重大差異。除其他外,這些因素包括與項目開發相關的風險;對額外融資的需求;與採礦和礦物加工相關的運營風險;礦產和商品價格的波動;所有權事項;環境責任索賠和保險;對關鍵人員的依賴;沒有分紅;競爭;稀釋;普通股價格和交易量的波動;以及政府實體的影響。前瞻性陳述是根據管理層在陳述發表之日的信念、估計和觀點做出的,如果這些信念、估計和觀點或其他情況發生變化,公司沒有義務更新前瞻性陳述。提醒投資者不要將不必要的確定性歸因於前瞻性陳述
Appendix A
附錄 A
Table 1: Assay Results: Tyko 2023 Drill Results from the West Pickle Area of Tyko I Property
表 1: 化驗結果:Tyko I 地產 West Pickle 地區的 Tyko 2023 年鑽探結果
Hole | Rock Type | From (m) |
To (m) |
Width (m) |
Ni % |
Cu % |
Co % |
TPM g/t (Pd+Pt+Au) |
Pd g/t |
Pt g/t |
Au g/t |
TK23-123 | Tonalite | No Significant Mineralization | |||||||||
TK23-124 | Ultramafic | 27.0 | 31.6 | 4.6 | 0.10 | 0.01 | 0.01 | 0.04 | 0.02 | 0.02 | 0.00 |
TK23-125 | Ultramafic | 17.0 | 27.0 | 10.0 | 0.10 | 0.02 | 0.01 | 0.00 | 0.00 | 0.00 | 0.00 |
38.7 | 46.0 | 7.3 | 0.10 | 0.01 | 0.01 | 0.03 | 0.01 | 0.01 | 0.00 | ||
134.6 | 142.0 | 7.4 | 0.12 | 0.01 | 0.01 | 0.03 | 0.01 | 0.02 | 0.00 | ||
TK23-126 | Ultramafic | 11.3 | 13.0 | 1.7 | 0.10 | 0.02 | 0.01 | 0.00 | 0.00 | 0.00 | 0.00 |
TK23-127 | Ultramafic | 34.1 | 53.0 | 18.9 | 0.11 | 0.02 | 0.01 | 0.03 | 0.01 | 0.02 | 0.00 |
TK23-128 | Ultramafic | 13.7 | 16.4 | 2.7 | 0.43 | 0.17 | 0.01 | 0.12 | 0.05 | 0.06 | 0.00 |
13.7 | 14.6 | 0.9 | 1.05 | 0.43 | 0.02 | 0.29 | 0.13 | 0.15 | 0.01 | ||
TK23-129 | Ultramafic | 28.0 | 31.5 | 3.5 | 0.13 | 0.04 | 0.01 | 0.01 | 0.00 | 0.01 | 0.00 |
TK23-130 | Tonalite | No Significant Mineralization | |||||||||
TK23-131 | Ultramafic | 18.0 | 41.0 | 23.0 | 0.11 | 0.03 | 0.01 | 0.01 | 0.00 | 0.01 | 0.00 |
TK23-132 | Ultramafic | 7.4 | 77.5 | 70.1 | 0.10 | 0.01 | 0.01 | 0.04 | 0.02 | 0.02 | 0.00 |
TK23-133 | Tonalite | No Significant Mineralization | |||||||||
TK23-134 | Ultramafic | 108.8 | 110.3 | 1.5 | 1.80 | 0.96 | 0.04 | 0.44 | 0.32 | 0.10 | 0.02 |
109.5 | 110.3 | 0.8 | 2.64 | 1.35 | 0.05 | 0.45 | 0.30 | 0.13 | 0.01 |
洞 | 搖滾類型 | 來自 (m) |
到 (m) |
寬度 (m) |
Ni % |
銅 % |
有限公司 % |
TPM g/t (鈀+鉑+金) |
Pd g/t |
Pt g/t |
Au g/t |
TK23-123 | Tonalite | 沒有明顯的礦化 | |||||||||
TK23-124 | Ultramaf | 27.0 | 31.6 | 4.6 | 0.10 | 0.01 | 0.01 | 0.04 | 0.02 | 0.02 | 0.00 |
TK23-125 | Ultramaf | 17.0 | 27.0 | 10.0 | 0.10 | 0.02 | 0.01 | 0.00 | 0.00 | 0.00 | 0.00 |
38.7 | 46.0 | 7.3 | 0.10 | 0.01 | 0.01 | 0.03 | 0.01 | 0.01 | 0.00 | ||
134.6 | 142.0 | 7.4 | 0.12 | 0.01 | 0.01 | 0.03 | 0.01 | 0.02 | 0.00 | ||
TK23-126 | Ultramaf | 11.3 | 13.0 | 1.7 | 0.10 | 0.02 | 0.01 | 0.00 | 0.00 | 0.00 | 0.00 |
TK23-127 | Ultramaf | 34.1 | 53.0 | 18.9 | 0.11 | 0.02 | 0.01 | 0.03 | 0.01 | 0.02 | 0.00 |
TK23-128 | Ultramaf | 13.7 | 16.4 | 2.7 | 0.43 | 0.17 | 0.01 | 0.12 | 0.05 | 0.06 | 0.00 |
13.7 | 14.6 | 0.9 | 1.05 | 0.43 | 0.02 | 0.29 | 0.13 | 0.15 | 0.01 | ||
TK23-129 | Ultramaf | 28.0 | 31.5 | 3.5 | 0.13 | 0.04 | 0.01 | 0.01 | 0.00 | 0.01 | 0.00 |
TK23-130 | Tonalite | 沒有明顯的礦化 | |||||||||
TK23-131 | Ultramaf | 18.0 | 41.0 | 23.0 | 0.11 | 0.03 | 0.01 | 0.01 | 0.00 | 0.01 | 0.00 |
TK23-132 | Ultramaf | 7.4 | 77.5 | 70.1 | 0.10 | 0.01 | 0.01 | 0.04 | 0.02 | 0.02 | 0.00 |
TK23-133 | Tonalite | 沒有明顯的礦化 | |||||||||
TK23-134 | Ultramaf | 108.8 | 110.3 | 1.5 | 1.80 | 0.96 | 0.04 | 0.44 | 0.32 | 0.10 | 0.02 |
109.5 | 110.3 | 0.8 | 2.64 | 1.35 | 0.05 | 0.45 | 0.30 | 0.13 | 0.01 |
(1) Reported widths are "drilled widths" not true widths.
(1) 報告的寬度是 “鑽孔寬度”,而不是真實寬度。
Table 2: Drill Hole Locations for assay results from this News Release
表 2: 本新聞稿中的化驗結果的鑽孔位置
Hole | Azimuth | Dip | Length | NAD83 z16 East | NAD83 z16 North | Elevation |
TK23-123 | 125.3 | -45 | 159.0 | 599360.0 | 5421973.0 | 344.0 |
TK23-124 | 177.4 | -45 | 153.0 | 602914.7 | 5421732.0 | 349.5 |
TK23-125 | 179.4 | -45 | 150.0 | 602910.4 | 5421871.0 | 350.7 |
TK23-126 | 180.0 | -45 | 30.5 | 603007.0 | 5421867.0 | 346.0 |
TK23-127 | 180.0 | -45 | 81.4 | 600785.9 | 5422590.0 | 368.6 |
TK23-128 | 179.1 | -50 | 171.0 | 600788.8 | 5422471.0 | 361.4 |
TK23-129 | 129.4 | -45 | 150.0 | 599548.5 | 5421606.0 | 332.4 |
TK23-130 | 181.6 | -45 | 126.0 | 600830.0 | 5422506.0 | 364.6 |
TK23-131 | 179.9 | -45 | 102.5 | 600732.1 | 5422499.0 | 363.5 |
TK23-132 | 179.8 | -45 | 120.0 | 600671.1 | 5422524.0 | 366.2 |
TK23-133 | 170.1 | -45 | 150.0 | 601767.3 | 5421957.0 | 348.2 |
TK23-134 | 144.0 | -58 | 147.0 | 601998.4 | 5421971.0 | 345.8 |
洞 | 方位角 | 浸 | 長度 | NAD83 z16 東方 | NAD83 z16 北方 | 海拔 |
TK23-123 | 125.3 | -45 | 159.0 | 599360.0 | 5421973.0 | 344.0 |
TK23-124 | 177.4 | -45 | 153.0 | 602914.7 | 5421732.0 | 349.5 |
TK23-125 | 179.4 | -45 | 150.0 | 602910.4 | 5421871.0 | 350.7 |
TK23-126 | 180.0 | -45 | 30.5 | 603007.0 | 5421867.0 | 346.0 |
TK23-127 | 180.0 | -45 | 81.4 | 600785.9 | 5422590.0 | 368.6 |
TK23-128 | 179.1 | -50 | 171.0 | 600788.8 | 5422471.0 | 361.4 |
TK23-129 | 129.4 | -45 | 150.0 | 599548.5 | 5421606.0 | 332.4 |
TK23-130 | 181.6 | -45 | 126.0 | 600830.0 | 5422506.0 | 364.6 |
TK23-131 | 179.9 | -45 | 102.5 | 600732.1 | 5422499.0 | 363.5 |
TK23-132 | 179.8 | -45 | 120.0 | 600671.1 | 5422524.0 | 366.2 |
TK23-133 | 170.1 | -45 | 150.0 | 601767.3 | 5421957.0 | 348.2 |
TK23-134 | 144.0 | -58 | 147.0 | 601998.4 | 5421971.0 | 345.8 |