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Taranis Intersects 279.6 G/t AgEq Over 2.86 M in Thunder Zone, and Gains Insight Into Deeper Targets at Thor

Taranis Intersects 279.6 G/t AgEq Over 2.86 M in Thunder Zone, and Gains Insight Into Deeper Targets at Thor

塔拉尼斯在 Thunder Zone 中穿越 279.6 g/t AgeQ 超過 2.86 米,並深入了解雷神更深的目標
Accesswire ·  2023/12/05 02:00

ESTES PARK, CO / ACCESSWIRE / December 4, 2023 / Taranis Resources Inc. ("Taranis" or the "Company") (TSX.V:TRO)(OTCQB:TNREF) is pleased to report on the first of five drill holes that were completed in the Thunder Zone at Thor in 2023.

科羅拉多州埃斯蒂斯公園/ACCESSWIRE/2023年12月4日/塔蘭尼斯資源公司(“塔拉尼斯” 或 “公司”)(TSX.V: TRO)(OTCQB: TNREF)很高興地報告2023年在雷神雷區完成的五個鑽孔中的第一個。

Exploratory drilling sought to improve understanding of the unique breccia-type mineralization found in the Thunder Zone, and its relationship to an underlying conductive body found on an airborne Mag/MT survey. Drilling in the Thunder Zone has been confined to a depth of 180 m below surface, and the top to the conductivity feature is estimated to lie 300 m below the surface. Although testing of the deeper target was planned for 2023, ongoing delays associated with a Notice of Work permit precluded exploration of this important target.

勘探性鑽探旨在增進對在雷區發現的獨特角礫岩型礦化及其與機載 mag/MT 調查中發現的潛在導電體的關係的理解。雷區鑽探僅限於地表以下 180 m 的深度,而電導率特徵的頂部估計位於地表以下 300 m 處。儘管計劃在2023年測試更深層次的目標,但與工作通知許可相關的持續延誤使人們無法對這一重要目標進行探索。

Thor-235 (-900)

Thor-235 (-90)0)

Drilling in the Thunder Zone continued to intersect mineralization under a rockslide on the south side of Thor's Ridge. Thor-235 was completed between previously reported drill holes Thor-231 (221 g/t AgEq over 17.9 m - including 1,355 g/t AgEq over 2.63 m) and Thor-220 (551.2 g/t AgEq over 3.96 m). Drilling in this area of the Thor deposit is difficult, and drill holes are commonly lost in the transition from rockslide to bedrock. The following table shows Thor-235 primarily intersected gold and zinc-related mineralization.

雷區鑽探繼續在雷神嶺南側的岩石滑坡下與礦化區相交。Thor-235是在先前報告的鑽孔Thor-231(超過17.9米的221 g/t AgeQ——包括超過2.63米的1,355 g/t AgeQ)和Thor-220(超過3.96米的551.2 g/t AgeQ)之間完成的。在雷神礦牀的這一區域鑽探很困難,在從岩石滑坡過渡到基岩的過程中,鑽孔通常會丟失。下表顯示 Thor-235 主要與金和鋅相關的礦化相交。

From (m)

To (m)

Interval (m)

Au (g/t)

Ag (g/t)

Cu(%)

Pb(%)

S(%)

Sb(%)

Zn(%)

AgEq

(g/t)

98.88

99.27

0.39

3.27

3.8

0.001

0.025

1.48

0.001

0.290

109.5

99.27

99.85

0.58

0.126

1.9

0.001

0.016

1.87

0.001

0.008

7.6

99.85

100.19

0.34

1.625

143.0

0.051

1.230

10.95

0.001

0.030

107.8

100.19

100.52

0.33

0.196

8.2

0.002

0.109

3.80

0.000

0.003

9.1

100.52

100.86

0.34

0.211

2.5

0.001

0.016

5.70

0.038

0.001

7.8

100.86

101.19

0.33

3.22

96.0

0.059

0.484

23.50

0.002

26.5

495.2

101.19

101.74

0.55

1.24

6.6

0.004

0.045

4.04

0.001

0.132

62.7

98.88-101.74

2.86

1.32

31.49

0.01

0.23

6.49

0.01

3.13

279.6

從 (m)

到 (m)

間隔 (m)

金 (g/t)

銀 (g/t)

銅 (%)

鉛 (%)

S (%)

Sb (%)

鋅 (%)

AgeQ

(g/t)

98.88

99.27

0.39

3.27

3.8

0.001

0.025

1.48

0.001

0.290

109.5

99.27

99.85

0.58

0.126

1.9

0.001

0.016

1.87

0.001

0.008

7.6

99.85

100.19

0.34

1.625

143.0

0.051

1.230

10.95

0.001

0.030

107.8

100.19

100.52

0.33

0.196

8.2

0.002

0.109

3.80

0.000

0.003

9.1

100.52

100.86

0.34

0.211

2.5

0.001

0.016

5.70

0.038

0.001

7.8

100.86

101.19

0.33

3.22

96.0

0.059

0.484

23.50

0.002

26.5

495.2

101.19

101.74

0.55

1.24

6.6

0.004

0.045

4.04

0.001

0.132

62.7

98.88-101.74

2.86

1.32

31.49

0.01

0.23

6.49

0.01

3.13

279.6

  • Indium is not included in the results, and results are pending.
  • 銦未包含在結果中,結果尚待確定。

Re-Examination of Drill Hole Thor-74

重新檢查鑽孔 Thor-74

Drill Hole Thor-74 was drilled in 2008 and targeted a positive magnetic anomaly that is adjacent to the Thor epithermal deposit. The drill hole failed to intersect any source responsible for the magnetic anomaly, and subsequent probing of the hole using a downhole magnetometer showed that Thor-74 passed directly over the source. Petrophysical testing of the core for this drill hole confirmed this interpretation, and a deeper drill hole will be required to identify the source of the anomaly. The anomaly is suspected to be related to a highly-altered mafic-volcanic unit (Jowett Formation) that is found along the main access road to Thor. Extensive petrology, geochemistry and hand-held spectrometer data has also indicated that this distinctive rock unit is potentially hornfels-related alteration peripheral to a deeper intrusive.

Thor-74 鑽孔於 2008 年鑽探,目標是雷神超熱礦牀附近的正磁異常。鑽孔未能與任何導致磁異常的源相交,隨後使用井下磁強計對該孔進行了探測,結果顯示Thor-74直接穿過了磁源。對該鑽孔岩心進行的岩石物理測試證實了這一解釋,因此需要更深的鑽孔才能確定異常的來源。該異常被懷疑與通往雷神的主要通道沿線發現的經過高度變化的魔法火山單元(Jowett Formation)有關。大量的岩石學、地球化學和手持式光譜儀數據也表明,這種獨特的岩石單元可能與角長巖相關,是深層侵入的邊緣。

Geochemical Rock Unit and Alteration Characterization at Thor

Thor的地球化學岩石單元和蝕變特徵

In 2022, Taranis undertook a comprehensive hand-held NIR/SWIR spectrometry survey of the property. This study was aimed at characterizing rock and alteration minerals on the project. Summer of 2023, Taranis conducted X-Ray Diffraction ("XRD") studies on specimens from around the property in order to validate the mineralogical results of the 2022 hand-held spectrometry survey. The results of the XRD study are ongoing and will be reported in the near future.

2022年,塔拉尼斯對該物業進行了全面的手持近紅外/短波紅外光譜調查。這項研究旨在表徵該項目中的岩石和蝕變礦物。2023年夏天,塔拉尼斯對來自該物業周圍的標本進行了X射線衍射(“XRD”)研究,以驗證2022年手持光譜調查的礦物學結果。XRD研究的結果正在進行中,並將在不久的將來公佈。

Thor geology is dominated by complexly folded meta-sedimentary rocks of the Sharon Creek and Broadview Formations, but within these rocks the original lithologies have been subject to various levels of hydrothermal alteration related to the precious and base metal emplacement. This alteration manifests itself in a number of ways, including differing colors, textures, and mineralogical changes. These are important to understand as they provide information that can be used to guide deep drilling to deeper intrusive targets.

雷神地質學以沙龍溪和布羅德維尤組中複雜摺疊的超沉積岩爲主,但在這些岩石中,原始巖性受到了與貴金屬和賤金屬陣地相關的不同程度的熱液變化。這種變化以多種方式表現出來,包括不同的顏色、質地和礦物學變化。理解這些信息很重要,因爲它們提供的信息可用於指導深度鑽探到更深的侵入性目標。

To gain better understanding of the alteration system at Thor, the Company also conducted an ultra-low level trace element study of the most common rock types found at Thor. Trace elements from each of the rock types were compared with samples from barren, unaltered sediments. This data shows, that apart from a large amount of sulphur (pyrite) being introduced into the host rocks at Thor around the epithermal deposit, there are a number of other trace elements that form a geochemical 'cloud' around the epithermal deposit. These elements include rhenium, cadmium, selenium, lead, copper, zinc, and gold. One notable element missing is silver and it appears to be tightly confined to the epithermal deposit within the epithermal quartz veins.

爲了更好地了解雷神的變化系統,該公司還對雷神發現的最常見的岩石類型進行了超低水平的微量元素研究。將每種岩石類型的微量元素與來自貧瘠、未改變的沉積物的樣本進行了比較。這些數據表明,除了大量的硫(黃鐵礦)被引入超熱礦牀周圍的托爾主巖中外,還有許多其他微量元素在超熱礦牀周圍形成地球化學 “雲”。這些元素包括、鎘、硒、鉛、銅、鋅和金。缺少的一個值得注意的元素是銀,它似乎僅限於超熱石英礦脈內的超熱礦牀。

Comment

評論

John Gardiner, President, and CEO of Taranis states "British Columbia's volcanic-hosted porphyry systems have well-documented and distinctive alteration patterns. It is unrealistic to assume that the intrusives that form these types of deposits were exclusively emplaced in volcanic rocks. Elsewhere, geologists are now asking what happens if these intrusives are emplaced in sedimentary rocks? Studies of alkalic porphyry deposits elsewhere in the world (Cadia Hill, Ridgeway) are now providing valuable insight into what the top of a concealed alkalic porphyry deposit looks like, and it does bear a resemblance to what we are seeing at Thor. The tops of alkalic porphyry bodies include epithermal deposits, widescale pyritization, illite-muscovite-carbonate (Au, Zn, Pb), and albite-K-feldspar-illite alteration. We believe that the Thor epithermal deposit which now extends for over 2 km at surface has a reason for being where it is - and that is an underlying intrusive body".

塔拉尼斯總裁兼首席執行官約翰·加德納表示:“不列顛哥倫比亞省的火山岩系統具有有據可查且獨特的變化模式。假設形成這類沉積物的侵入物完全位於火山岩中是不切實際的。在其他地方,地質學家現在在問,如果將這些侵入物放置在沉積岩中會發生什麼?對世界其他地方(Cadia Hill、Ridgeway)的鹼性斑岩沉積物的研究現在爲隱蔽的鹼性斑岩沉積物的頂部是什麼樣子提供了寶貴的見解,它確實與我們在雷神看到的相似。鹼性斑岩體的頂部包括超熱礦牀、大規模黃鐵化、伊利特-莫斯科維特-碳酸鹽(金、鋅、鉛)和Albite-k-Feldspar-Illite的變化。我們認爲,目前在地表延伸超過2千米的雷神超熱礦牀有其存在的理由,那是一個潛在的侵入體”。

Quality Control

質量控制

Core samples from the Thor Project are cut in half, and one-half of the sample is shipped to ALS Geochemistry ("ALS") Kamloops for preparation. Analyses are completed by ALS in Vancouver, which is accredited to ISO/IEC 17025:2017 general requirements for the competence of testing and calibration laboratories. Taranis also uses its own set of certified reference standards in the analytical stream every 10th sample as an additional quality control. Gold is determined using a one-tonne fire assay method, with an atomic absorption finish. Silver content is determined using Inductively Coupled Plasma Spectroscopy ("ICP"), and in cases where silver content exceeds 100 ppm, samples are reanalyzed where over limits are required. The content of other metals is also determined using ICP, and in cases where the metal content exceeds analytical limits, the sample is analyzed using ICP with a different set of calibration standards.

來自雷神項目的核心樣本被切成兩半,一半的樣本被運送到ALS地球化學(“ALS”)坎盧普斯進行製備。分析由位於溫哥華的 ALS 完成,該中心已獲得 ISO/IEC 17025:2017 測試和校準實驗室能力一般要求的認證。塔蘭尼斯還在分析流中每 10 次使用自己的一套經過認證的參考標準第四 樣品作爲額外的質量控制。金是使用一噸火分析法測定的,表面經過原子吸收。銀含量使用電感耦合等離子體光譜法(“ICP”)測定,如果銀含量超過100 ppm,則在需要超過限值的地方對樣品進行重新分析。其他金屬的含量也使用ICP測定,如果金屬含量超過分析極限,則使用ICP和一套不同的校準標準對樣品進行分析。

Silver Equivalent Calculation

白銀當量計算

Owing to the complex, polymetallic nature of the Thor epithermal deposit and the presence of at least five different metals that can potentially be recovered in the Mineral Resource, Taranis uses a method of reporting results called Silver Equivalent ("AgEq") to help readers understand exploration drilling results. These prices are based on January 2023 metal prices to facilitate comparison with prior drilling results.

由於托爾超熱礦牀的複雜多金屬性質以及礦產資源中至少存在五種不同的金屬可供回收,塔拉尼斯使用一種名爲銀當量(“AgeQ”)的報告結果的方法來幫助讀者了解勘探鑽探結果。這些價格基於2023年1月的金屬價格,以便於與之前的鑽探結果進行比較。

AgEq calculations use the following metal values: Gold US$61.03/gram, Silver US$0.76/gram, Copper US$9.19/kg, Zinc US$3.21/kg, Lead US$3.21/kg & Antimony US$5.60/kg. AgEq = [Ag (g/t) + (Au g/t * 80.63) + (Cu%*121.42) + (Zn%*42.41) + (Pb%*28.93) + (Sb%*73.99)]

AgeQ 使用以下金屬值進行計算:黃金61.03美元/克,白銀0.76美元/克,銅9.19美元/千克,鋅3.21美元/千克,鉛3.21美元/千克,銻每千克5.60美元。ageQ = [Ag (g/t) + (Au g/t * 80.63) + (Cu%*121.42) + (Zn%*42.41) + (Pb%*28.93) + (Sb%*73.99)]

Update on Petition Filed with Supreme Court of British Columbia

向不列顛哥倫比亞省最高法院提交的請願書的最新情況

As of the date of this News Release, the Province has not filed a response to the Company's Petition filed October 16th, 2023, concerning a Notice of Work application filed August 30th, 2022.

截至本新聞稿發佈之日,該省尚未對公司10月16日提交的申請作出回應第四,2023 年,涉及 8 月 30 日提交的工作通知申請第四,2022。

About Taranis Resources Inc.

關於塔拉尼斯資源公司

Taranis Resources Inc. is a well-positioned exploration company that is exploring and developing its 100%-owned Thor precious-base metal project in British Columbia. Taranis has drilled over 250 drill holes on the project, defining a near-surface epithermal deposit that is over 2 km long. The Company refers to the epithermal trend as the "Trunk," invoking the anatomy of an elephant to portray the connection of the epithermal deposit to the underlying Jumbo and Horton intrusive targets.

Taranis Resources Inc. 是一家定位良好的勘探公司,正在不列顛哥倫比亞省勘探和開發其100%擁有的Thor貴金屬項目。塔拉尼斯在該項目上鑽了250多個鑽孔,定義了一個長度超過2公里的近地表淺熱礦牀。該公司將超熱趨勢稱爲 “樹幹”,以大象的解剖結構來描繪超熱礦牀與潛在的巨型和霍頓侵入性目標之間的聯繫。

Qualified Person

合格人員

Exploration activities at Thor were overseen by John Gardiner (P. Geo.), who is a Qualified Person under the meaning of Canadian National Instrument 43-101. John Gardiner is a principal of John J. Gardiner & Associates, LLC which operates in British Columbia under Firm Permit Number 1002256.

雷神號的勘探活動由約翰·加德納(P. Geo.)監督,根據加拿大國家儀器43-101的定義,他是合格人員。約翰·加德納是 John J. Gardiner & Associates, LLC 的負責人,該公司在不列顛哥倫比亞省運營,公司許可證號爲 1002256。

For additional information on Taranis or its 100%-owned Thor project in British Columbia, visit

有關 Taranis 或其在不列顛哥倫比亞省 100% 所有的 Thor 項目的更多信息,請訪問

Taranis currently has 94,587,027 shares issued and outstanding (109,262,027 shares on a fully-diluted basis).

塔拉尼斯目前已發行和流通94,587,027股股票(全面攤薄後爲109,262,027股)。

TARANIS RESOURCES INC.

TARANIS RESOURCES INC

Per: John J. Gardiner (P. Geo.),
President and CEO

Per:John J. Gardiner(P. Geo.),
總裁兼首席執行官

For further information contact:

欲了解更多信息,請聯繫:

John J. Gardiner
681 Conifer Lane
Estes Park, Colorado
80517
Phone: (720) 209-3049
johnjgardiner@earthlink.net

約翰·J·加德納
681 Conifer Lane
科羅拉多州埃斯蒂斯公園
80517
電話:(720) 209-3049
johnjgardiner@earthlink.net

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 NEWS RELEASE.

多倫多證券交易所風險投資交易所及其監管服務提供商(該術語在多倫多證券交易所風險投資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 News Release may contain forward looking statements based on assumptions and judgments of management regarding future events or results that may prove to be inaccurate as a result of factors beyond its control, and actual results may differ materially from expected results.

本新聞稿可能包含基於管理層對未來事件或結果的假設和判斷的前瞻性陳述,這些事件或結果可能由於其無法控制的因素而被證明是不準確的,並且實際結果可能與預期結果存在重大差異。

SOURCE: Taranis Resources, Inc.

來源:塔拉尼斯資源公司


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