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RETRANSMISSION: Beyond Lithium Discovers New Spodumene Bearing Pegmatite Zone at Ear Falls Project in Northwest Ontario

RETRANSMISSION: Beyond Lithium Discovers New Spodumene Bearing Pegmatite Zone at Ear Falls Project in Northwest Ontario

重傳:Beyond Lithium 在安大略省西北部的 Ear Falls 項目中發現了新的含鋰輝石的偉晶岩帶
newsfile ·  2023/09/18 20:45

Samples Up To 4.54% Li2O Along 3 Km Long Zone

沿3公里長的區域採樣高達4.54%的Li2O

HIGHLIGHTS

高光

  • New spodumene bearing pegmatites zone discovered at the Ear Falls Project with grab samples up to 4.54% Li2O.
  • Favorable geology and a highly fractionated sample located 2 km northeast of the new discovery spodumene zone suggest the potential for a minimum 3-km-long trend for exploration of spodumene bearing pegmatites.
  • The discovered spodumene-bearing pegmatites are located along a structurally controlled zone of 1 km in strike length, open in all directions.
  • Exploration plan has been submitted to Ontario's Ministry of Mines for a stripping and a drilling program in October.
  • Ear Falls Project was expanded from 3,375 ha to 20,623 ha (~600% expansion) upon the successful discovery of the new spodumene bearing pegmatites zone for a cash cost per hectare of only $7.98.
  • The eastern expansion of the project provides a new exploration opportunity to search for a potentially identical geological system.
  • 在Eear Falls專案中發現了新的含鋰輝石偉晶巖帶,採集的樣品中Li2O含量高達4.54%。
  • 有利的地質條件和位於新發現的鋰輝石帶東北2公里處的高分餾樣品表明,勘探含鋰輝石偉晶巖的趨勢至少有3公里長。
  • 已發現的含鋰輝石偉晶巖沿一條走向長度為1公里的構造控制帶分佈,走向四面八方。
  • 勘探計劃已提交給安大略省礦業部,以便在10月份進行剝離和鑽探計劃。
  • 在成功發現新的鋰輝石偉晶巖帶後,Ear Falls專案從3,375公頃擴大到20,623公頃(~600%),每公頃現金成本僅為7.98美元。
  • 該專案的東擴為尋找潛在相同的地質系統提供了新的勘探機會。

Winnipeg, Manitoba--(Newsfile Corp. - September 18, 2023) - Beyond Lithium Inc. (CSE: BY) (OTCQB: BYDMF) (the "Company" or "Beyond Lithium") is pleased to announce the discovery of a new spodumene-bearing pegmatite zone at its 206 sq. km Ear Falls Project in Northwest Ontario. Grab samples have assayed up to 4.54% Li2O and a minimum 3-km-long prospective trend has been identified. A highly fractionated sample located 2 km northeast of the spodumene pegmatite zone establishes a minimum of 3 km long trend for spodumene bearing pegmatites exploration.

溫尼伯,馬尼託巴省-(Newsfile Corp.-2023年9月18日)-Beyond Lithium Inc.(CSE:BY)(OTCQB:BYDMF)(The公司“或”超越鋰)很高興地宣佈,在其位於安大略省西北部的206平方公里的耳朵瀑布專案中發現了一個新的含鋰輝石偉晶巖帶。抓取樣品的檢測結果表明,Li的含量高達4.54%2.O並且已經確定了至少3公里長的預期趨勢。一個位於鋰輝石偉晶巖帶東北2公里處的高分餾樣品為含鋰輝石偉晶巖的勘探確立了至少3公里的趨勢。

Upon making this new discovery, Beyond Lithium strategically expanded the Ear Falls Project from 3,375 ha to 20,623 ha (~600% expansion) in area (Figure 1).

在獲得這一新發現後,Beyond Li戰略性地將Eear Falls專案的面積從3,375公頃擴大到20,623公頃(~600%的擴張)(圖1)。


Figure 1. Ear Falls Project Expanded Claims Map


圖1.EAR Falls專案擴展索賠地圖

The Ear Falls Project, previously referred to as the Wenasaga Property, is located right outside the town of Ear Falls, 70 km south of Red Lake and 145 km north of Dryden in Northwest Ontario. Ear Falls has excellent infrastructure including highway and logging road access, power lines, services, and local labour.

Ear Falls專案以前稱為韋納薩加物業,位於安大略省西北部Ear Falls鎮外,紅湖以南70公里,Dryden以北145公里。耳瀑布擁有一流的基礎設施,包括駭維金屬加工和伐木道路通道、電力線、服務和當地勞動力。

Mr. Lawrence Tsang, VP Exploration for Beyond Lithium commented: "This spodumene discovery is significant as it occurs within a 13-km-long metasedimentary-granite structural corridor where there's opportunity for more discoveries as we ramp up exploration. We are targeting subparallel spodumene pegmatite dykes along the main metasedimentary-batholith structure and the major regional fault. Exploration on the eastern expansion of the project also provides an opportunity to search for a potentially identical geological system."

Beyond Lithium勘探副總裁勞倫斯·曾先生評論說:“鋰輝石的發現意義重大,因為它位於13公里長的變質-花崗巖構造走廊內,隨著我們加大勘探力度,將有機會發現更多的鋰輝石偉晶巖脈。我們的目標是沿著主要的變質-岩基構造和主要的區域斷層尋找次平行的鋰輝石偉晶巖脈。對專案東部擴展的勘探也提供了一個尋找潛在相同的地質系統的機會。”

Mr. Tsang added that "Exploration at the Ear Falls Project is ongoing, and we have already submitted an exploration plan with Ontario's Ministry of Mines to carry out a stripping and a drilling program to further delineate the spodumene pegmatites zone. The stripping and drilling program is targeted to commence in October."

曾先生補充說:“Ear Falls專案的勘探正在進行中,我們已經向安大略省礦業部提交了一份勘探計劃,以實施剝離和鑽探計劃,以進一步圈定鋰輝石偉晶巖帶。剝離和鑽探計劃計劃於10月份開始。”


Figure 2. Overview Exploration Trend at the Ear Falls Project Showing the 3 km trend of Spodumene/Beryl Zone (black arrow) and a 13 km long Metasedimentary-Granite Structural Corridor (red polygon outline) and a Potential Subparallel Structure (blue polygon outline)


圖2.耳朵瀑布專案的勘探趨勢概述,顯示鋰輝石/綠柱石帶(黑色箭頭)和13公里長的變質沉積-花崗巖構造走廊(紅色多邊形輪廓)和潛在的次平行結構(藍色多邊形輪廓)的趨勢

Allan Frame, President & CEO, commented that "This exciting news supports that new discoveries are possible outside of the remote regions of northern Quebec and Ontario. With just three months into our 2023 exploration program trying to cover all 64 projects with over 150,000 ha in area, Beyond Lithium has made two major discoveries in Ontario: the Allen Graeme pluton at Cosgrave and this new high grade spodumene bearing pegmatites zone at the Ear Falls Project. This early success shows the effectiveness of our exploration program. Many assay results remain to be received and announced and we are confident in delivering additional positive results before the end of the year."

總裁首席執行官艾倫·弗萊姆評論說:“這一令人振奮的消息支持在魁北克北部和安大略省偏遠地區以外有可能發現新的發現。我們的2023年勘探計劃僅進行了三個月,就試圖覆蓋所有64個專案,面積超過150,000公頃,Beyond Li在安大略省已經有了兩個重大發現:科斯格雷夫的Allen Graeme巖體和Ear Falls專案的這一新的高品位鋰輝石偉晶巖帶。這一初步成功表明了我們勘探計劃的有效性。許多分析結果有待收到和公佈,我們有信心在年底前帶來更多積極的結果。”

Mr. Frame added: "In a recent news release I mentioned that it is important for our shareholders to keep in mind that while we are as anxious as they are to share all assay results as they come in, it is sometimes a better course of action to first consolidate our land position either through staking, optioning or both in certain districts. I am proud to report that this approach has allowed us to acquire 17,233 additional hectares around the discovery announced today at an average cash cost of $7.98 per hectare and the issuance of only 300,000 shares."

弗萊克補充說:“在最近的一次新聞稿中,我提到,重要的是我們的股東要記住,雖然我們和他們一樣急於分享所有的化驗結果,但有時更好的做法是首先鞏固我們的土地地位,要麼是通過在某些地區進行配售,要麼是通過兩者兼而有之。我很自豪地告訴大家,這種方法讓我們在今天宣佈的發現周圍額外獲得了17233公頃土地,平均現金成本為每公頃7.98美元,只發行了30萬股。”

The finding of the spodumene pegmatites zone by Beyond Lithium at the Ear Falls project is a brand-new discovery in this region. Beyond Lithium recognized the potential of this area and was able to stake most of the prospective open grounds around the original claims and consolidated additional claims from a few prospectors to assemble a contiguous project of 20,623 ha in area.

Beyond Lithium在Ear Falls專案中發現的鋰輝石偉晶巖帶是該地區的一項全新發現。Beyond Lithium認識到了這一地區的潛力,能夠圍繞最初的主張建立大部分預期的空地,並整合了幾個探礦者的額外主張,以組裝一個面積為20,623公頃的連續專案。

The expansion has delineated two high priority areas for exploration associated with the labels in Figure 3 below:

擴展劃定了與下面圖3中的標籤相關聯的兩個高優先勘探區域:

1- Explore along the main metasedimentary-batholith structure and the major regional fault and look for subparallel spodumene pegmatite dykes.

1-沿著主要的變質沉積-岩基構造和主要的區域斷裂進行勘探,尋找次平行的鋰輝偉晶巖牆。

2- Explore for additional prospective structure along the newly mapped metasedimentary-batholith in the northwest and look for additional spodumene pegmatite dykes.

2-沿著西北部新繪製的變質沉積巖基尋找更多的遠景構造,尋找更多的鋰輝偉晶巖牆。


Figure 3. Overview of the High Priority Areas for Exploration at the Ear Falls Project


圖3.EAR Falls專案高度優先勘探區域概覽

Background of the spodumene discovery

鋰輝石發現的背景

The Phase 1 exploration program at the Ear Falls Project was completed in June. We have since updated the geology of the project and more significantly located the batholith-metasedimentary contact within the project as this contact is probably the preferential structure for LCT pegmatites (Figure 4). After discovering the spodumene pegmatites zone, Beyond Lithium's field team further explored along this metasedimentary-batholith contact and was able to locate three new beryl bearing pegmatites (Figure 4).

Ear Falls專案的第一階段勘探計劃於6月份完成。自那以後,我們更新了該專案的地質情況,更重要的是在該專案中找到了岩基-變質沉積接觸,因為該接觸可能是LCT偉晶巖的優先結構(圖4)。在發現鋰輝石偉晶巖帶後,Beyond Lithium的野外團隊沿著這一變質沉積-岩基接觸帶進一步探索,並找到了三個新的含綠柱石的偉晶巖(圖4)。


Figure 4. Phase 1 Mapping of the Ear Falls Project with the Spodumene Pegmatites Zone and the 3 New Beryl Pegmatites Discovered Along the Metasedimentary and the Granite Contact


圖4.沿變沉積和花崗巖接觸面發現的鋰輝石偉晶巖帶和3個新的綠柱石偉晶巖的耳朵瀑布專案的第一階段地圖

Subparallel spodumene bearing pegmatites along a minimum of 1 km strike length were discovered along the main logging road of the Ear Falls Project up to 6 meters wide in exposed outcrops (Figure 6). The spodumene pegmatites are hosted in both granite and metasediment trending generally at 40 to 60 degrees following the regional foliation with local variabilities. These spodumene pegmatites are covered by a thin layer of vegetation. A follow-up stripping program has been planned to include the removal of the overburden to further outline the true thickness and the density of these spodumene pegmatites.

沿著耳朵瀑布專案的主要伐木道路,在裸露的露頭中發現了含有至少1公里走向長度的次平行鋰輝石偉晶巖(圖6)。鋰輝偉晶巖賦存於花崗巖和變質巖中,總體趨勢為40~60度,遵循區域面理,具有局部變異性。這些鋰輝石偉晶巖被一層薄薄的植被覆蓋。後續剝離計劃計劃包括去除覆蓋層,以進一步勾勒出這些鋰輝石偉晶巖的真實厚度和密度。

Sampling and assay results

抽樣和化驗結果

A total of 205 individual pegmatite outcrops have now been mapped along the main structural corridor to date illustrated as blue dots in Figure 8 and we have collected 68 samples at the project. So far, 48 of the samples have received assays. From the 48 assays, four samples were taken from the spodumene pegmatites zone with Li2O ranging from 0.76% to 4.54% and cesium ranging from 32.83 ppm to 68.97 ppm (Table 1). More samplings including channel sampling are planned on the beryl and the spodumene pegmatites by the end of September to early October to further outline the lithium bearing zone.

到目前為止,沿著主要構造走廊總共繪製了205個偉晶巖露頭的地圖,如圖8中的藍點所示,我們在該專案中收集了68個樣本。到目前為止,已有48個樣本接受了化驗。在48次化驗中,有4次樣品是與Li一起從鋰輝石偉晶巖帶中提取的2.O為0.76%至4.54%,銫為32.83ppm至68.97ppm(表1)。計劃在9月底至10月初對綠柱石和鋰輝石偉晶巖進行更多的採樣,包括通道採樣,以進一步勾勒出含鋰帶。


Figure 5. Spodumene Crystals in Pegmatite


圖5.偉晶巖中的鋰輝石晶體

Mineralogy
Sample ID Easting Northing Lithology QTZ KSPAR MUS BIO GARNET TOUR BERYL SPOD Cs ppm Li2O %
E00105585 483944 5620144 PEG 1 1 68.97 0.76
E00105886 483770 5620063 PEG 1 1 1 1 1 52.24 2.28
E00105887 483743 5620021 PEG 1 1 1 1 1 37.76 4.54
E00105892 483340 5619761 PEG 1 1 1 1 1 32.83 3.90
* Li2O%=Li ppm*2.153/10,000
礦物學
樣本ID 向東 北距 巖性 QTZ KSPAR 毛斯 生物 石榴石 遊覽 綠柱石 鷹架 CS ppm Li2O%
E00105585 483944 5620144 釘釘 1 1 68.97 0.76
E00105886 483770 5620063 釘釘 1 1 1 1 1 52.24 2.28
E00105887 483743 5620021 釘釘 1 1 1 1 1 37.76 4.54
E00105892 483340 5619761 釘釘 1 1 1 1 1 32.83 3.90
*Li2O%=Li百萬分率*2.153/萬

Table 1 Assays Results of the 4 Grab Samples from the Spodumene Pegmatites Zone

表1分析了鋰輝石偉晶巖帶的4個抓取樣品的結果


Figure 6. Assays of Spodumene Pegmatites Zone


圖6.鋰輝石偉晶巖帶的分析

A couple of samples, E00105586 and E00105888, were collected just meters away from the spodumene pegmatites in the granite and metasediment host rocks. These two samples in the host rocks show significantly elevated Cs, 134 ppm and 636 ppm, and Li ,408 ppm and 1407 ppm, respectively (Table 2). In addition, the Cs values in the host rock or the alteration halo of the spodumene mineralization (134 and 636ppm Cs) are much higher than the Wenasaga Lake batholith (average of 7ppm Cs) implies the melt is highly enriched in incompatible rare elements and volatiles for the formation of lithium bearing pegmatites which has gone through a high level of fractionation (Breaks 2003) (Figure 7). This geochem baseline in the host rock with elevated Cs and Li could be the alteration halo signature of the spodumene pegmatites at the Ear Falls Project. This signature would be a great exploration tool for exploring blind target in the area.

在距花崗巖和變質母巖中鋰輝石偉晶巖僅幾米處採集了E00105586和E00105888兩個樣品。寄主岩石中這兩個樣品的Cs顯著升高,分別為134ppm和636ppm,Li的Cs分別為408ppm和1407ppm(表2)。此外,容礦岩石或鋰輝石礦化蝕變暈中的Cs值(134和636ppm Cs)遠高於韋納薩加湖基岩(平均Cs值為7ppm),這意味著熔體高度富含不相容的稀有元素和揮發分,從而形成經歷了高度分餾的含鋰偉晶巖(Break 2003)(圖7)。圍巖中Cs和Li含量升高的地化基線可能是耳垂工程鋰輝石偉晶巖的蝕變暈標誌。這一特徵將是探索該地區盲目目標的一個很好的勘探工具。

Sample ID Easting Northing Lithology Cs ppm Li ppm
E00105586 483944 5620144 GRA 134 408
E00105888 483741 5620022 MSED 636 1407
樣本ID 向東 北距 巖性 CS ppm Li ppm
E00105586 483944 5620144 格拉 一百三十四 四百零八
E00105888 483741 5620022 MSED 六百三十六 1407

Table 2 Assays Results of Grab Samples from Host Rocks of the Spodumene Pegmatites Zone

表2鋰輝石偉晶巖帶寄主岩石抓取結果分析

Geological interpretation

地質解釋

Cesium versus K/Rb variation in samples is a common and convenient diagram to display the fractionation trend or the relative degree of evolution of S-type, peraluminous granites and related pegmatite granites and the rare-element pegmatite groups that fractionated from the parent granitic rocks. With increasing fractionation of the pegmatite-forming melt, the compositions of the potassium feldspar and mica become more enriched in rubidium and cesium thus the fractionation trend point to the lower right corner in the plot as the higher fractionated area. By plotting up the K/Rb vs Cs values of the 48 completed assays, a distinctive fractionation trend progresses from the SW to the NE orientation with an increase in Cs and a decrease in K/Rb ratio (Figure 7). One sample, E00105574, is plotted in the higher fractionated quadrant of the plot and this sample is located 2 km northeast on trend of the spodumene zone (Figures 2 & 3).

樣品中Cs隨K/Rb的變化是顯示S型花崗巖、過鋁花崗巖及其相關偉晶花崗巖和從母花崗巖中分餾出來的稀有元素偉晶巖群的分餾趨勢或相對演化程度的一種常用且方便的圖解。隨著偉晶巖形成熔體分餾程度的增加,鉀長石和雲母的成分變得更加富含Rb和Cs,因此分餾趨勢指向地塊右下角作為分餾較高的區域。通過繪製48個已完成分析的K/Rb與Cs的值,一個明顯的分餾趨勢是從西南向NE方向進行的,Cs增加,K/Rb比率降低(圖7)。一個樣品E00105574被繪製在地塊的較高分餾象限,該樣品位於鋰輝石帶走向東北2公里處(圖2和圖3)。


Figure 7. K/Rb vs Cs Plot of Ear Falls Project Compared to the Wenasaga Lake Batholith & Fractionation Trend with the Higher Fractionated Sample located 2 km NE of the Spodumene Pegmatites Zone


圖7.耳瀑布專案與韋納薩加湖岩基的K/Rb-Cs圖比較&分餾程度較高的樣品位於鋰輝偉晶巖帶東北方向2公里處

Regional geological context

區域地質背景

The Ontario Geological Survey's released collected data in 2002 and outlined a couple of 1.1% and 1.2% A/CNK ratio samples in the eastern expansion of the Ear Falls project which suggested the presence of a nearby fertile pluton (Tindle 2002). Based on LCT pegmatites literature, a molecular ratio [Al2O3/(CaO + Na2O + K2O)] is commonly used to indicate whether a sample or a stock/pluton is mildly peraluminous (A/CNK = 1.0 to 1.1) or strongly peraluminous (A/CNK > 1.2) (Tindle 2006). These mildly to strongly peraluminous A/CNK samples also coincide with an area of elevated deep lake sediment in lithium just situated northeast from the Ear Falls project (Figure 8). This eastern expansion could be a new area to explore for a separate system than the new spodumene pegmatites zone associated with the Wenasaga Lake batholith and the Sandy Creek beryl pegmatites group.

安大略省地質調查局公佈了2002年收集的數據,並概述了Ear Falls專案東部擴張地區的幾個A/CNK比為1.1%和1.2%的樣品,這表明附近存在一個富饒的巖體(Tindle 2002)。根據LCT偉晶巖文獻,分子比[Al_2O_3/(CaO+Na2O+K_2O)]通常用來指示樣品或礦體/巖體是中等過鋁(A/CNK=1.0~1.1)還是強過鋁(A/CNK>1.2)(Tindle 2006)。這些溫和到強烈過鋁的A/CNK樣品也與位於耳瀑布專案東北方向的鋰深湖沉積隆起區域相吻合(圖8)。這一東部擴張可能是一個新的區域,可以探索一個獨立的系統,而不是與韋納薩加湖基岩和沙溪綠柱石偉晶巖群有關的新的鋰輝石偉晶巖帶。


Figure 8. Brand New Exploration Target in the Eastern Area of the Expanded Ear Falls Project with >1% A/CNK and Elevated Lake Sediment in Lithium


圖8.擴大耳瀑布專案東部地區全新的勘探目標,A/CNK>1%,鋰湖沉積物升高

Beyond Lithium acknowledges the effort and work preformed by the project vendors, Bounty Gold Corp and Last Resort Resources, that led to the first discovery of its kind around the fertile Wenasaga Lake batholith and provides a proof of concept for the methodology used to assemble for the 64 prospective projects. Notably, Beyond Lithium's Ogani Lake Project is located just 30 km northeast of the Ear Falls Project and 65 km west of Green Technology Metals' (ASX: GT1) Root and McCombe Lithium deposits. The Ogani Lake Project was also recently expanded from 1,427 hectares to 5,177 hectares after beryl was found in several white tourmaline-muscovite pegmatites up to 10 meters wide during Beyond Lithium's phase 1 program (Figure 9).

Beyond Lithium承認專案供應商Bounty Gold Corp和Last Resort Resources所做的努力和工作,導致在肥沃的韋納薩加湖基岩周圍首次發現此類專案,並為為64個預期專案組裝所使用的方法提供了概念證明。值得注意的是,Beyond Lithium的Ogani Lake專案位於Ear Falls專案東北30公里處,Green Technology Metals(ASX:GT1)Root和McCombe鋰礦藏以西65公里處。在Beyond Li專案第一階段期間,在幾塊寬達10米的白色電氣石-白雲母偉晶中發現了綠柱石,Ogani湖專案最近也從1,427公頃擴大到5,177公頃(圖9)。


Figure 9. Beyond Lithium's Projects in the Area of the North Caribou Terrane & English River Subprovince District in Relation to the Green Technologies Metals' (ASX: GT1) Root-McComb Lithium Deposits


圖9.Beyond Lithium在北加勒比地區的專案與Green Technologies Metals(ASX:GT1)Root-McComb鋰礦藏的關係

Regionally, the Wenasaga Lake batholith was described as a S-type fertile pluton which is likely the parental pluton of the Sandy Creek beryl pegmatites. The Sandy Creek beryl bearing pegmatites that were discovered in the early 1960s are located 7 km southwest of the new spodumene pegmatites zone (Breaks 1993). Very limited to no exploration work was done in the area since the discovery of the Sandy Creek beryl pegmatites for over 60 years. Beyond Lithium recognized this area to be favourable for LCT pegmatites because there are a well-established Wenasaga Lake batholith as the potential source of LCT pegmatites of the area and the higher fractionated Sandy Creek beryl occurrence in the area that led Beyond Lithium's field crew discovering the new spodumene pegmatites zone.

在區域上,韋納薩加湖基岩被描述為S型可育巖體,很可能是沙溪綠柱石偉晶巖的母巖。20世紀60年代初發現的沙溪綠柱石偉晶巖位於新的鋰輝石偉晶巖帶西南7公里處(BREAKS 1993)。自從發現沙溪綠柱石偉晶巖60多年以來,該地區沒有進行過任何勘探工作。Beyond Li認為這一地區有利於LCT偉晶巖,因為該地區有一個著名的韋納薩加湖岩基作為LCT偉晶巖的潛在來源,而且該地區有較高分級的沙溪綠柱石產出,這導致Lithium的野外工作人員發現了新的鋰輝石偉晶巖帶。

Based on the geochem plot of the 2023's collected samples in comparison with the batholith and the Sandy Creek beryl pegmatites (Figure 7), the Wenasaga Lake batholith is likely the parental pluton of the new spodumene bearing pegmatites zone. The batholith was mapped concordant to the Uchi-English River sub provincial boundary covering approximately 260km2 in area (Breaks 2003). The Sandy Creek beryl bearing pegmatites were noted to follow this regional foliation orientation of the host metasedimentary rock (Breaks 1993). This regional NE structure is an ideal host and fluid pathway for the formation and fractionation of LCT pegmatites as most LCT pegmatites deposits in the world have some sort of structural control for its formation (Bradley 2017).

根據2023年S採集的樣品與基岩和沙溪綠柱石偉晶巖的地化圖(圖7),韋納薩加湖基岩很可能是新的鋰輝石偉晶巖帶的母巖體。基岩的測繪與烏奇-英格利斯河的省以下分界線一致,面積約為260平方公里(見2003年)。含有砂溪綠柱石的偉晶巖被髮現遵循寄主變質沉積巖的這一區域面理方向(Break 1993)。這一區域北東向構造是LCT偉晶巖形成和分餾的理想寄主和流體通道,因為世界上大多數LCT偉晶巖礦床對其形成具有某種構造控制(Bradley 2017)。

Sources

消息來源

1 Breaks, F.W. and Bond, W.D., 1993. The English River Subprovince - An Archean Gneiss Belt: Geology, Geochemistry and associated mineralization; Ontario Geological Survey, Open File Report 5846, v.1, p.1-483, 884p.

1 Break,F.W.和Bond,W.D.,1993。英吉利河次省-太古宙片麻岩帶:地質學、地球化學和相關礦化;安大略省地質調查,公開檔案報告5846,v.1,p.1-483,884頁。

2 Breaks, F.W., Selway, J.B. and Tindle, A.G. 2003. Fertile peraluminous granites and related rare-element mineralization in pegmatites, Superior Province, northwest and northeast Ontario: Operation Treasure Hunt; Ontario Geological Survey, Open File Report 6099, 179p.

2 Break,F.W.,Selway,J.B.和Tindle,A.G.2003。安大略省西北部和東北部優勝省偉晶巖中富饒的過鋁花崗巖和相關的稀有元素礦化:尋寶行動;安大略省地質調查局,開放檔案報告6099,179頁。

3 Tindle, A.G., Selway, J.B. and Breaks, F.W. 2002. Electron microprobe and bulk analyses of fertile peraluminous granites and related rare-element pegmatites, Superior Province, northwest and northeast Ontario: Operation Treasure Hunt; Ontario Geological Survey, Miscellaneous Release-Data 111

3 Tindle,A.G.,Selway,J.B.and Break,2002年6月。安大略省優勝省、安大略省西北部和東北部富饒的過鋁花崗巖和相關稀土偉晶巖的電子探針和塊體分析:尋寶行動;安大略省地質調查局,雜項發佈-數據111

4 Tindle, A.G., Selway, J.B. and Breaks, F.W. 2006. Electron microprobe and bulk rock and mineral compositions of barren and fertile peraluminous granitic rocks and rare-element pegmatites, northcentral and northeastern Superior Province of Ontario; Ontario Geological Survey, Miscellaneous Release-Data 210.

4 Tindle,A.G.,Selway,J.B.and Break,F.W.2006。安大略省中北部和東北部貧瘠和肥沃的過鋁花崗巖和稀有元素偉晶巖的電子探針和大塊岩石和礦物組成;安大略省地質調查局,雜項發佈-數據210。

5 Bradley, D.C., McCauley, A.D., and Stillings, L.M., 2017, Mineral-deposit model for lithium-cesium-tantalum pegmatites: U.S. Geological Survey Scientific Investigations Report 2010-5070-O, 48 p.,

5布拉德利,哥倫比亞特區,麥考利,A.D.和斯蒂林斯,L.M.,2017,鋰銫鉭偉晶巖的礦藏模型:美國地質調查局科學調查報告2010-5070-O,48頁,

6 Breaks, F.W. and Bond, W.D., 1993. The English River Subprovince - An Archean Gneiss Belt: Geology, Geochemistry and associated mineralization; Ontario Geological Survey, Open File Report 5846, v.1, p.1-483, 884p.

6休息,F.W.和邦德,W.D.,1993。英吉利河次省-太古宙片麻岩帶:地質學、地球化學和相關礦化;安大略省地質調查,公開檔案報告5846,v.1,p.1-483,884頁。

6 Green Technology Metals (ASX: GT1)

6綠色科技金屬(ASX:GT1)

Quality Assurance/Quality Control

品質保證/質量控制

All collected rock samples were put in sturdy plastic bags, tagged, and sealed at site. Sample bags were then put in rice bags and kept securely before being sent by road transport or delivered by the crew supervisor to SGS's preparation facility in Red Lake or Sudbury, Ontario, for sample preparation. Pulps are analyzed at the SGS facility in Burnaby, BC. All samples are analyzed with Four-Acid Digestion/Combined ICP-AES/MS package (49 elements). Samples with lithium overlimit (>10,000 ppm Li) are analyzed with another Four-Acid Digestion with higher detection limit of up to 10% Li. Batches of samples with overlimit >10,000 ppm or 1% Li are analyzed with Sodium Peroxide Fusion for validation. The QA/QC protocol included the insertion and monitoring of appropriate reference materials, in this case high concentration and low concentration certified OREAS and CDN lithium standards to validate the accuracy and precision of the assay results.

所有采集的岩石樣本都被放入堅固的塑膠袋中,貼上標籤,並在現場密封。樣品袋隨後被放入米袋並安全保存,然後通過公路運輸或由船員主管運送到SGS位於紅湖或安大略省薩德伯裡的準備設施進行樣品準備。紙漿在不列顛哥倫比亞省伯納比的SGS設施進行分析。所有樣品均採用四酸消解/電感耦合等離子體發射光譜/質譜儀聯用(49種元素)分析。鋰超標(>10,000 ppm Li)樣品用另一種四酸消解進行分析,檢出限最高可達10%Li。超限>10,000 ppm或1%Li的批次樣品用過氧化鈉熔融進行分析以進行驗證。品質保證/質量控制方案包括插入和監測適當的標準物質,在這種情況下,高濃度和低濃度認證的OREAS和CDN鋰標準,以驗證分析結果的準確性和精密度。

Qualified Person and Third-Party Data

合格人員和第三方數據

The scientific and technical information in this news release has been reviewed and approved by Lawrence Tsang, P.Geo., VP Exploration of the Company. Lawrence Tsang is a "qualified person" as defined in National Instrument 43-101 - Standards of Disclosure for Mineral Projects.

本新聞稿中的科學和技術資訊已由公司勘探副總裁勞倫斯·曾俊華審閱和批准。曾俊華是《國家文書43-101》所界定的“合資格人士”-《礦產專案資訊披露標準》

About Beyond Lithium Inc.

Beyond Lithium Inc.簡介

Beyond Lithium Inc. is the largest greenfield lithium exploration player in Ontario with 64 high potential greenfield lithium properties totalling over 150,000 hectares. The Company has adopted the project generator business model to maximize funds available for exploration projects, while minimizing shareholder dilution. Beyond Lithium is advancing certain of its projects with its exploration team and will seek to option other properties to joint venture partners. Partnering on various projects will provide a source of non-dilutive working capital, partner-funded exploration, and long-term residual exposure to exploration success.

Beyond Lithium Inc.是安大略省最大的綠地鋰勘探公司,擁有64處高潛力的綠地鋰礦,總面積超過150,000公頃。公司採用了專案生成者的商業模式,以最大限度地增加勘探專案的可用資金,同時最大限度地減少股東的稀釋。Beyond Lithium正在與其勘探團隊推進某些專案,並將尋求將其他資產選擇給合資夥伴。與不同專案的合作將提供非稀釋營運資本、合作夥伴資助的勘探以及勘探成功的長期剩餘敞口。

Beyond Lithium currently has 28,259,658 common shares outstanding.
Please follow @BeyondLithium on Twitter, Facebook, LinkedIn, Instagram and YouTube.

Beyond Lithium目前擁有28,259,658股已發行普通股。
請關注@BeyondLithium on推特FacebookLinkedInInstagramYouTube

For more information, please refer to the Company's website at

欲瞭解更多資訊,請訪問公司網站

CAUTIONARY STATEMENT REGARDING FORWARD-LOOKING INFORMATION: This news release includes certain "forward-looking information" within the meaning of applicable Canadian securities legislation. All statements, other than statements of historical fact, included herein including, without limitation, statements regarding future capital expenditures, anticipated content, commencement, and cost of exploration programs in respect of the Company's projects and mineral properties, anticipated exploration program results from exploration activities, resources and/or reserves on the Company's projects and mineral properties, and the anticipated business plans and timing of future activities of the Company, are forward-looking information. Although the Company believes that such statements are reasonable, it can give no assurance that such expectations will prove to be correct. Often, but not always, forward-looking information can be identified by words such as "pro forma", "plans", "expects", "will", "may", "should", "budget", "scheduled", "estimates", "forecasts", "intends", "anticipates", "believes", "potential" or variations of such words including negative variations thereof, and phrases that refer to certain actions, events or results that may, could, would, might or will occur or be taken or achieved. In stating the forward-looking information in this news release, the Company has applied several material assumptions, including without limitation, that market fundamentals will result in sustained precious and base metals demand and prices, the receipt of any necessary permits, licenses and regulatory approvals in connection with the future exploration of the Company's properties, the availability of financing on suitable terms, and the Company's ability to comply with environmental, health and safety laws.

有關前瞻性資訊的警告性聲明:本新聞稿包括適用於加拿大證券法的某些“前瞻性資訊”。除有關歷史事實的表述外,本文中包含的所有表述,包括但不限於有關公司專案和礦產的未來資本支出、預期內容、開工和成本、勘探活動的預期勘探計劃結果、公司專案和礦產的資源和/或儲量,以及公司未來活動的預期業務計劃和時間的表述,均為前瞻性資訊。儘管該公司相信這樣的陳述是合理的,但它不能保證這種預期將被證明是正確的。前瞻性資訊常常但不總是可以用諸如“形式”、“計劃”、“預期”、“將”、“可能”、“應該”、“預算”、“預定”、“估計”、“預測”、“打算”、“預期”、“相信”、“潛在”等詞語或這些詞語的變體,包括其負面變化,以及提及可能、可能、將、可能或將發生或將發生或將採取或實現的某些行動、事件或結果的短語來識別。在本新聞稿中陳述前瞻性資訊時,公司應用了幾個重大假設,包括但不限於,市場基本面將導致貴金屬和賤金屬的需求和價格持續增長,獲得與公司未來資產勘探有關的任何必要的許可證、許可證和監管批准,以合適的條款獲得融資,以及公司遵守環境、健康和安全法律的能力。

Forward-looking information involves known and unknown risks, uncertainties and other factors which may cause the actual results, performance or achievements of the Company to differ materially from any future results, performance or achievements expressed or implied by the statements of forward-looking information. Such risks and other factors include, among others, statements as to the anticipated business plans and timing of future activities of the Company, the proposed expenditures for exploration work on its properties, the ability of the Company to obtain sufficient financing to fund its business activities and plans, delays in obtaining governmental and regulatory approvals (including of the Canadian Securities Exchange), permits or financing, changes in laws, regulations and policies affecting mining operations, risks relating to epidemics or pandemics such as COVID-19, the Company's limited operating history, currency fluctuations, title disputes or claims, environmental issues and liabilities, as well as those factors discussed under the heading "Risk Factors" in the Company's prospectus dated February 23, 2022 and other filings of the Company with the Canadian securities regulatory authorities, copies of which can be found under the Company's profile on the SEDAR website at .

前瞻性資訊涉及已知和未知的風險、不確定性和其他因素,這些風險、不確定性和其他因素可能導致公司的實際結果、業績或成就與前瞻性資訊陳述中明示或暗示的任何未來結果、業績或成就大不相同。此類風險和其他因素包括但不限於有關公司預期的業務計劃和未來活動的時間安排、公司物業勘探工作的擬議支出、公司獲得足夠資金為其業務活動和計劃提供資金的能力、在獲得政府和監管機構批准(包括加拿大證券交易所)、許可或融資方面的延誤、影響採礦作業的法律、法規和政策的變化、與流行病或流行病(如新冠肺炎)有關的風險、公司有限的運營歷史、貨幣波動、所有權糾紛或索賠、環境問題和債務。以及在公司日期為2022年2月23日的招股說明書和公司提交給加拿大證券監管機構的其他檔案中“風險因素”項下討論的因素,這些檔案的副本可在SEDAR網站上的公司簡介中找到。

Readers are cautioned not to place undue reliance on forward-looking information. The Company undertakes no obligation to update any of the forward-looking information in this news release except as otherwise required by law.

告誡讀者不要過度依賴前瞻性資訊。除法律另有要求外,本公司不承擔更新本新聞稿中任何前瞻性資訊的義務。

For further information, please contact:

如需更多資訊,請聯繫:

Allan Frame
President and CEO
Tel: 403-470-8450
Email: allan.frame@beyondLithium.ca

Allan框架
總裁與首席執行官
電話:403-470-8450
電子郵件:allan.Frame@byondLithium.ca

Jason Frame
Manager of Communications
Tel: 587-225-2599
Email: jason.frame@beyondLithium.ca

賈森·費雷爾
傳播部經理
電話:587-225-2599
電子郵件:jason.Frame@byondLithium.ca

To view the source version of this press release, please visit

要查看本新聞稿的源版本,請訪問

譯文內容由第三人軟體翻譯。


以上內容僅用作資訊或教育之目的,不構成與富途相關的任何投資建議。富途竭力但無法保證上述全部內容的真實性、準確性和原創性。
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