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Brixton Metals Discovers Multiple Porphyry Systems at the North Target on Its Thorn Project

Brixton Metals Discovers Multiple Porphyry Systems at the North Target on Its Thorn Project

Brixton Metals在其Thorn項目的北方靶區發現了多個斑岩系統。
GlobeNewswire ·  2024/12/16 20:30

VANCOUVER, British Columbia, Dec. 16, 2024 (GLOBE NEWSWIRE) -- Brixton Metals Corporation (TSX-V: BBB, OTCQB: BBBXF) (the "Company" or "Brixton") is pleased to announce North Target drill hole results of the 2024 season from its wholly owned Thorn Project located in NW British Columbia, Canada. The Thorn Project is an underexplored copper-gold porphyry district with many large scale exploration target areas identified.

溫哥華,不列顛哥倫比亞省,2024年12月16日(全球Newswire)-- Brixton Metals Corporation(TSX-V: BBb,OTCQB: BBBXF)(「公司」或「Brixton」)很高興地宣佈其在加拿大不列顛哥倫比亞省西北部的全資託恩項目的2024年度北目標鑽孔結果。託恩項目是一個尚未深入探查的銅金斑岩區,已確定多個大規模探索目標區域。

Highlights

亮點

  • Brixton Metals' maiden drill program at the North Target has intercepted a Mo-Cu porphyry system with mineralization starting from surface consisting of:
    • Multiple generations of porphyry-style quartz and quartz-anhydrite veins hosting molybdenite, pyrite, and chalcopyrite accompanied by potassic alteration halos
    • Anomalous copper and molybdenum within multi-kilometer scale alteration zones of phyllic, potassic, and propylitic alteration centered around multi-phase crowded porphyritic diorites
  • A ground magnetotelluric geophysical survey has identified numerous conductive features that correlate with zones of hydrothermal alteration
  • Geochronology sampling highlights discovery potential of Thorn Project with multiple metallogenic epochs identified
  • Brixton Metals在北目標的首次鑽探計劃截獲了一個鉬銅斑岩系統,礦化自地表開始,包括:
    • 多代斑岩風格的石英和石英-脫水石膏脈,伴有鉬礦、黃鐵礦和黃銅礦,以及鉀礦化邊緣。
    • 在數公里規模的礦化遠景帶內發現異常的銅和鉬,礦化類型包括親水性、鉀質和綠泥石質改造,集中在多相擁擠的斑岩花崗岩中心。
  • 一項地面磁流體電磁地球物理勘探已識別出許多導電特徵,這些特徵與熱液改造區域相關。
  • 地質年代學取樣突顯了索恩項目的發現潛力,識別出多個成礦時代。

Vice President of Exploration, Christina Anstey, stated, "The results from the North Target highlight the extraordinary discovery potential of the Thorn Project. Intersecting multiple porphyry systems in an area that has seen minimal historical exploration is a testament to the strength of our technical approach. These early findings not only confirm the presence of a robust mineralized system, but also set the stage for further exploration to uncover higher-grade zones and additional targets across this expansive and underexplored district."

探索副總裁Christina Anstey表示:「來自北目標的結果突顯了索恩項目的非凡發現潛力。在一個歷史探礦極少的地區交匯多個花崗岩體系統,證明了我們技術方案的強大。這些早期發現不僅確認了一個強大礦化系統的存在,還是進一步探索以發現更高品位礦區及其他標的的基礎,這個地區廣闊且未充分探索。」

Figure 1. Thorn Project Location Map with Copper Geochemistry.

圖1:帶銅地球化學的Thorn項目位置圖。

Table 1. Select Assay Intervals for Drilling at the North Target.

表1. 北目標鑽探選擇的分析區間。

Hole ID From (m) To (m) Interval (m) Mo (%) Cu (%)
THN24-312 12.00 650.00 638.00 0.023 0.04
including 401.00 650.00 249.00 0.028 0.03
including 595.00 650.00 55.00 0.047 0.05
THN24-313 12.00 421.00 409.00 0.013 0.06
including 202.40 219.28 16.88 0.019 0.11
and including 275.00 294.00 19.00 0.011 0.12
THN24-296 491.00 530.00 39.00 0.005 0.04
THN24-298 No Significant Results
孔 ID 從(米) 到(米) 間隔(米) 鉬(%) 銅 (%)
THN24-312 12.00 650.00 638.00 0.023 0.04
包括 401.00 650.00 249.00 0.028 0.03
包括 595.00 650.00 55.00 0.047 0.05
THN24-313 12.00 421.00 409.00 0.013 0.06
包括 202.40 219.28 16.88 0.019 0.11
包括 275.00 294.00 19.00 0.011 0.12
THN24-296 491.00 530.00 39.00 0.005 0.04
THN24-298 沒有顯著結果

HQ size core samples were cut in half and sampled predominantly at 1.5m intervals. Assay values are weighted averages. The true width of the mineralized intervals has not yet been determined.

HQ尺寸的核心樣本被切成兩半,並主要在150萬的間隔內採樣。化驗值是加權平均數。礦化間隔的實際寬度尚未確定。

Figure 2. Plan Map for the North Target.

圖2. 北部目標的平面圖.

Figure 3. Plan Map for the North Target with 2024 MT Geophysical Survey at 300m depth below surface.

圖3. 北部靶區的規劃圖,2024年Mt地球物理勘測,深度爲30000萬以下。

Technical Discussion

技術討論

The North Target is located approximately 10km northwest of the Camp Creek Porphyry Target. Prior to the 2024 field season, exploration at the North Target has been limited to small and sporadic surficial sampling programs and has never been drilled. Through compilation of historic work and geological mapping by Brixton Metals, multiple porphyry, epithermal, and skarn mineral occurrences accompanied by large alteration footprints have been identified within a north-northwest trending 11km by 4km area, highlighting the potential for a large mineral system. The North Target is underlain by Stuhini Group upper Triassic mafic volcanics and Laberge Group lower Jurassic sedimentary rocks. These units are intruded by multiple Late Cretaceous to Eocene intrusions.

北部靶區位於Camp Creek斑岩靶區西北約10公里處。在2024年實地勘探季節之前,北部靶區的勘探僅限於小規模和零散的地表取樣計劃,且從未鑽探。通過Brixton Metals對歷史工作和地質圖的彙編,識別出多個斑岩、熱液和角閃巖礦牀,伴隨着大規模的蝕變足跡,存在於北北西走向的11公里乘以4公里的區域內,突顯出大型礦牀系統的潛力。北部靶區的基底是Stuhini Group上三疊世的鎂鐵質火山岩和Laberge Group下侏羅世的沉積岩。這些單元被多個晚白堊世至始新世的侵入體所侵入。

The 2024 field season commenced with a SPARTAN Magnetotelluric (MT) geophysical survey consisting of a 108 station grid with 1-kilometer spacing. This was followed up by 4 drill holes at the Wild Moly and Main Gossan target areas for a total of 2,266m.

2024年實地勘探季節以SPARTAN磁通量(MT)地球物理勘測開始,涵蓋108個站點的網格,間距爲1公里。隨後在Wild Moly和Main Gossan靶區進行了4個鑽孔,總計226600萬。

Wild Moly

野生鉬

Wild Moly has a surface expression of strong quartz-sericite-pyrite alteration with quartz-molybdenite-chalcopyrite veins and a coincident low resistivity feature identified from the MT survey. This target was tested with two drill holes for a total of 1,071m leading to the discovery of a previously unrecognized Mo-Cu porphyry system. While copper grades average 0.04% in THN24-312 and 0.06% in THN24-313, narrow intervals have returned >0.1% Cu and further work will evaluate the potential for zones of higher-grade copper. With an at least 1.8km by 1.2km area of phyllic alteration mapped at surface, the system remains open in all directions.

野生鉬的表面表現出強烈的石英—白雲母—黃鐵礦蝕變,伴有石英—鉬礦—銅礦脈,並且在Mt調查中識別出一個低電阻特徵。這個目標通過兩個鑽孔進行了測試,總計107100萬,發現了一個之前未被識別的鉬—銅斑岩系統。儘管THN24-312的銅平均品位爲0.04%,THN24-313爲0.06%,但窄間隔的樣本返回了>0.1%的銅,進一步的工作將評估高品位銅區的潛力。表面測繪出至少1.8公里乘1.2公里的高鉀蝕變區,該系統在所有方向上仍然開放。

THN24-312 was drilled at an azimuth of 128.2 degrees, a dip -65.0 degrees, and to a depth of 650m, targeting the highest density of mapped quartz veins and center of the low resistivity anomaly. The drill hole collared into a crowded biotite-quartz-feldspar diorite porphyry from surface to 602.85m where Stuhini mafic volcanic tuffs and breccias were intersected until end of hole. Mineralization occurs in quartz-anhydrite veins with pyrite-molybdenite and rare chalcopyrite. Potassium feldspar and biotite alteration forms halos to veins with a pervasive sericite-pyrite overprint. THN24-312 returned 638.00m of 0.023% Mo, 0.04% Cu from 12.00m, including 55.00m of 0.047% Mo, 0.05% Cu from 595.00m.

THN24-312的鑽孔方位爲128.2度,傾角爲-65.0度,深度達到65000萬,目標是勘測到的石英礦脈的最高密度和低電阻異常的中心位置。鑽孔自表面進入一個擁擠的黑雲母—石英—長石輝綠岩斑岩,直到60285萬處,交會了Stuhini基性火山灰和角礫岩,直到孔的結束。礦化發生在石英—無水石膏脈中,並伴隨有黃鐵礦—鉬礦和稀有的銅礦。鉀長石和黑雲母的蝕變形成了脈的光環,展示出廣泛的白雲母—黃鐵礦的覆蓋。THN24-312返回了63800萬的0.023%鉬和0.04%銅,從1200萬處,包括59500萬的0.047%鉬和0.05%銅。

Figure 4. Photos of Mineralized HQ-Sized Drill Core from THN24-312.

圖4. THN24-312的礦化HQ尺寸鑽芯照片。

THN24-313 was drilled from the same pad and collared at an azimuth 308.1 degrees, a dip of -65.1 degrees, and to a depth of 421m, testing a copper-in-soil anomaly. The hole collared into the diorite porphyry until 116.35m where the lithology became Stuhini mafic volcanic dominant with sub-50m intervals of porphyry. As with THN24-312, porphyry-style mineralized quartz veins with potassic halos were intersected throughout until alteration became chlorite-epidote-magnetite-pyrite dominant at depth where it is interpreted that the hole transitioned to the margins of the porphyry system. THN24-313 returned 409.00m of 0.013% Mo, 0.06% Cu from 12.00m, including 19.00m of 0.12% Cu, 0.011% Mo from 275.00m. The best copper values occur within mafic volcanics at the contact with the diorite porphyry.

THN24-313在同一平台鑽探,方位角爲308.1度,傾斜度爲-65.1度,深度達到42100萬,測試了土壤中的銅異常。鑽孔進入二長巖鑲嵌巖,直到11635萬,巖性變爲Stuhini基性火山岩主導,並伴有少於-5000萬的鑲嵌巖區間。與THN24-312一樣,貫穿整個鑽孔的礦化石英脈與鉀質暈交匯,直到在深度上改變爲綠泥石-榴石-磁鐵礦-黃鐵礦主導,其中解釋爲鑽孔過渡到鑲嵌巖系統的邊緣。THN24-313返回了40900萬的0.013%鉬,0.06%銅,從1200萬起,包括從27500萬的1900萬中獲取的0.12%銅,0.011%鉬。最優的銅值發生在與二長巖鑲嵌巖接觸的基性火山岩中。

Figure 5. Photos of Mineralized HQ-Sized Drill Core from THN24-313.

圖5. THN24-313礦化HQ尺寸鑽芯的照片。

Figure 6. Cross-Section of Wild Moly Drill Holes.

圖6. Wild Moly鑽孔的橫截面。

Main Gossan

主要礦化帶

The Main Gossan consists of a 2.5km by 3.2km altered area with propylitic, sericitic, and locally potassic alteration assemblages, widespread pyrite, and isolated occurrences of chalcopyrite, copper oxides, and molybdenite at surface. It is underlain by Laberge Group sedimentary rocks which are cut by multiple intrusive phases. The Main Gossan was tested with two holes totaling 1,195m targeting areas where porphyry-style quartz veins were observed on surface with a coincident northeast trending conductive feature. The 2024 drilling has confirmed the presence of a porphyry system at the Main Gossan.

主礦脈由一個2.5公里乘3.2公里的改造區域組成,具有輝綠岩、閃石和局部富鉀的改造組合,廣泛的黃鐵礦,以及表面孤立出現的銅礦礦石、銅氧化物和鉬礦石。其下方爲拉貝爾格集團沉積岩,穿插多次侵入相。主礦脈通過兩個總計119500萬的探孔進行了測試,目標是觀察到表面有斑岩型石英脈的區域,並具有一致的東北走向的導電特徵。2024年的鑽探證實了主礦脈存在斑岩礦牀。

THN24-296 was collared at an azimuth of 159.5 degrees, a dip of -68.8 degrees, and to a depth of 530m and THN24-298 was collared from the same pad at an azimuth of 245.1 degrees, dip of -60 degrees, and to a depth of 665m. Both holes collared into Laberge mudstone to conglomerate horizons which are intruded by a hornblende-biotite-quartz-feldspar diorite porphyry. Chlorite-epidote-magnetite-pyrite was the dominant alteration assemblage with structurally controlled zones of sericite-pyrite overprint. Mineralization consisted of disseminated pyrite, commonly >5%, with rare quartz-molybdenite and quartz-sphalerite-galena-chalcopyrite veins. Both holes ended in an intrusive breccia with elevated copper values, including THN24-296 which returned 39.00m of 0.04% Cu and 0.005% Mo from 492.50 meters to end of hole. While the Main Gossan holes returned no significant intercepts, the widespread propylitic alteration suggests drilling intersected the margins of a concealed porphyry system.

THN24-296的起鑽方位爲159.5度,傾角爲-68.8度,深度爲53000萬,而THN24-298來自同一鑽孔,方位爲245.1度,傾角爲-60度,深度爲66500萬。兩個探孔均鑽入拉貝爾格頁岩至礫岩地層,受到角閃石-黑雲母-石英-長石輝長岩斑岩的侵入。氯英石-綠泥石-磁鐵礦-黃鐵礦是主要的改造組合,具有結構控制的白雲母-黃鐵礦疊加區。礦化包括分散的黃鐵礦,通常大於5%,並有稀有的石英-鉬礦石和石英-閃鋅礦-方鉛礦-黃銅礦脈。兩個孔最終均爲侵入性角礫岩,銅值升高,包括THN24-296在492.50米至結束孔之間返回3900萬的0.04%銅和0.005%鉬。儘管主礦脈的探孔未回採到顯著的截面,但廣泛的輝綠岩改造暗示鑽探截交了一個隱蔽的斑岩礦牀的邊緣。

Figure 7. Photos of Mineralized HQ-Sized Drill Core from THN24-296.

圖7. 來自THN24-296的礦化HQ尺寸鑽芯照片。

Figure 8. Photos of Mineralized HQ-Sized Drill Core from THN24-298.

圖8. 來自THN24-298的礦化HQ尺寸鑽芯照片。

Figure 9. Cross-Section of Main Gossan Drill Holes.

圖9. 主礦脊鑽孔的橫截面。

Geophysics

地球物理學

The MT survey has identified numerous near-surface conductive features across the target area. With the survey successfully highlighting the Wild Moly porphyry discovery as a resistivity low, further ground-truthing of other anomalies is planned for the 2025 field season. One resistive feature of interest is a 3km wide donut-shaped conductor located at the south end of the target area (Figure 3). The flanks of the conductor correspond with quartz-sericite-pyrite alteration and the central portion is interpreted to be covered by post-mineral volcanics. The geophysical data will be further evaluated and will incorporate petrophysical properties collected on drill core and surface samples into a constrained inversion.

Mt調查已在目標區域識別出許多近地表的導電特徵。 該調查成功地將Wild Moly斑岩發現標記爲電阻低,計劃在2025年野外季節進一步確認其他異常。 一處感興趣的電阻特徵是位於目標區域南端的一個寬3公里的甜甜圈狀導體(圖3)。導體的兩側與石英-絹雲母-黃鐵礦蝕變相對應,中央部分被解釋爲覆蓋在礦後火山岩下。地球物理數據將進一步評估,並將結合在鑽芯和地表樣本中收集的岩石物理特性進行約束反演。

Geochronology

地質年代學

A Re-Os geochronology sample from a molybdenite vein at the Main Gossan has returned an age date of 58 +/- 0.2 Ma. While mineralization at the Main Gossan and Wild Moly are interpreted to be Paleocene in age, 3km south of the Main Gossan, U-Pb zircon age dating of a porphyritic intrusion with weak chalcopyrite mineralization has returned 85.5 +/- 0.7 Ma, coeval with the mineralizing PX porphyry at the Camp Creek Porphyry Target. Along with known Late Triassic mineralization in the central portions of the property and Neogene epithermal mineralization adjacent to the Thorn Project at Newmont's Hearts Peak Property, these results highlight the discovery potential of the area with multiple metallogenic epochs identified.

A Re-Os geochronology sample from a molybdenite vein at the Main Gossan has returned an age date of 58 +/- 0.2 Ma. While mineralization at the Main Gossan and Wild Moly are interpreted to be Paleocene in age, 3km south of the Main Gossan, U-Pb zircon age dating of a porphyritic intrusion with weak chalcopyrite mineralization has returned 85.5 +/- 0.7 Ma, coeval with the mineralizing PX porphyry at the Camp Creek Porphyry Target. Along with known Late Triassic mineralization in the central portions of the property and Neogene epithermal mineralization adjacent to the Thorn Project at Newmont's Hearts Peak Property, these results highlight the discovery potential of the area with multiple metallogenic epochs identified.

Conclusion

結論

The 2024 exploration program at the North Target has been successful through the integration of multiple dataset types into a maiden drill program that intersected a molybdenum-copper porphyry at the Wild Moly and the margins of a porphyry system at the Main Gossan. With only a small portion of the 11km by 4km area of porphyry style alteration tested, further work will utilize geochemistry from surface and drilling data, hyperspectral data, and geophysics to target for other porphyry centers.

The 2024 exploration program at the North Target has been successful through the integration of multiple dataset types into a Maiden drill program that intersected a molybdenum-copper porphyry at the Wild Moly and the margins of a porphyry system at the Main Gossan. With only a small portion of the 11km by 4km area of porphyry style alteration tested, further work will utilize geochemistry from surface and drilling data, hyperspectral data, and geophysics to target for other porphyry centers.

Table 2. Collar Information for 2024 North Target Drilling.

Table 2. Collar Information for 2024 North Target Drilling.

Hole ID Easting Northing Elevation (m) Azimuth Dip Depth (m)
THN24-296 620134 6503632 1244 159.5 -68.8 530.00
THN24-298 620130 6503633 1243 245.1 -60.0 665.00
THN24-312 619989 6507802 894 128.2 -65.0 650.00
THN24-313 619984 6507807 897 308.1 -65.1 421.00
孔 ID 東座標 北座標 海拔(米) 方位 傾斜 深度(米)
THN24-296 620134 6503632 1244 159.5 -68.8 530.00
THN24-298 620130 6503633 1243 245.1 -60.0 665.00
THN24-312 619989 6507802 894 128.2 -65.0 650.00
THN24-313 619984 6507807 897 308.1 -65.1 421.00

Quality Assurance & Quality Control

Quality Assurance & Quality Control

Quality assurance and quality control protocols for drill core sampling was developed by Brixton. Core samples were mostly taken at 1.5m intervals. Blank, duplicate (lab pulp) and certified reference materials were inserted into the sample stream for at least every 20 drill core samples. Core samples were cut in half, bagged, zip-tied and sent directly to ALS Minerals preparation facility in Whitehorse, Yukon or Langley, British Columbia depending on available lab capacity. ALS Minerals Laboratories is registered to ISO 9001:2008 and ISO 17025 accreditations for laboratory procedures. Samples were analyzed at ALS Laboratory Facilities in North Vancouver, British Columbia for gold by fire assay with an atomic absorption finish, whereas Ag, Pb, Cu and Zn and 48 additional elements were analyzed using four acid digestion with an ICP-MS finish. Over limits for gold were analyzed using fire assay and gravimetric finish. The standards, certified reference materials, were acquired from CDN Resource Laboratories Ltd., of Langley, British Columbia and the standards inserted varied depending on the type and abundance of mineralization visually observed in the primary sample. Blank material used consisted of non-mineralized siliceous landscaping rock. A copy of the QAQC protocols can be viewed at the Company's website.

Brixton制定了鑽芯取樣的質量保證和質量控制協議。核心樣本大多按150萬的間隔取樣。每20個鑽芯樣本中至少插入一個空白樣本、一個重複樣本(實驗室粉末)和經認證的參考材料。核心樣本被切成兩半,裝袋,用拉鍊綁好,直接送往位於育空省懷特霍斯或不列顛哥倫比亞省蘭裏市的ALS礦業準備設施,具體取決於實驗室的可用能力。ALS礦業實驗室已獲得ISO 9001:2008和ISO 17025實驗室程序的註冊認證。樣本在不列顛哥倫比亞省北溫哥華的ALS實驗室設施中進行金的火焰熔鍊分析,使用原子吸收結束,而銀、鉛、銅、鋅及48種額外元素通過四酸消化和ICP-MS結束進行分析。金的超限樣本通過火焰熔鍊和重量分析進行分析。標準化的經認證參考材料由不列顛哥倫比亞省蘭裏市的CDN資源實驗室有限公司獲取,而插入的標準材料根據在原始樣本中目測到的礦化類型和豐度而有所不同。使用的空白材料由非礦化的硅質園藝石組成。公司的官網上可以查看QAQC協議的副本。

Qualified Person (QP)

Qualified Person (QP)

Mr. Daniel Guestrin, P.Geo., is a Senior Project Geologist for the Company who is a qualified person as defined by National Instrument 43-101. Mr. Guestrin has verified the referenced data and analytical results disclosed in this press release and has approved the technical information presented herein.

丹尼爾·古斯特林先生,P.Geo.,是本公司的高級項目地質學家,滿足國家儀器43-101定義的合格人士要求。古斯特林先生已核實本新聞稿中披露的參考數據和分析結果,並批准此處呈現的技術信息。

About Brixton Metals Corporation

關於Brixton Metals Corporation

Brixton Metals is a Canadian exploration company focused on the advancement of its mining projects. Brixton wholly owns four exploration projects: Brixton's flagship Thorn copper-gold-silver-molybdenum Project, the Hog Heaven copper-silver-gold Project in NW Montana, USA, which is optioned to Ivanhoe Electric Inc., the Langis-HudBay silver-cobalt-nickel Project in Ontario and the Atlin Goldfields Project located in northwest BC which is optioned to Eldorado Gold Corporation. Brixton Metals Corporation shares trade on the TSX-V under the ticker symbol BBB, and on the OTCQB under the ticker symbol BBBXF. For more information about Brixton, please visit our website at .

布里克斯頓金屬是一家加拿大的勘探公司,專注於推進其採礦項目。布里克斯頓全資擁有四個勘探項目:布里克斯頓旗艦的松露銅-黃金-白銀-鉬項目,位於美國蒙大拿州西北部的霍格天堂銅-銀-黃金項目,該項目已轉讓給伊凡霍電氣公司;安大略省的Langis-HudBay銀-鈷-鎳項目;以及位於不列顛哥倫比亞省西北部的Atlin Goldfields項目,該項目已轉讓給埃爾多拉多黃金公司。布里克斯頓金屬公司的股票在TSX-V交易,股票代碼爲BBb,並在OTCQb交易,股票代碼爲BBBXF。有關布里克斯頓的更多信息,請訪問我們的官方網站。 .

On Behalf of the Board of Directors

董事會代表

Mr. Gary R. Thompson, Chairman and CEO

加里·R·湯普森先生,董事長兼首席執行官

For Investor Relations inquiries please contact: Mr. Michael Rapsch, Senior Manager, Investor Relations. email: michael.rapsch@brixtonmetals.com or call: 604-630-9707

如需投資者關係的諮詢,請聯繫:邁克爾·拉普施先生,投資者關係高級經理。電子郵件:michael.rapsch@brixtonmetals.com 或致電:604-630-9707

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 release.

TSX創業公司交易所或其監管服務提供商(如TSX創業公司政策中定義的那樣)不對本公告的充分性或準確性負責。

Information set forth in this news release may involve forward-looking statements under applicable securities laws. Forward-looking statements are statements that relate to future, not past, events. In this context, forward-looking statements often address 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, including statements that address potential quantity and/or grade of minerals, potential size and expansion of a mineralized zone, proposed timing of exploration and development plans, or other similar expressions. All statements, other than statements of historical fact included herein including, without limitation, statements regarding the use of proceeds. 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, the following risks: the need for additional financing; operational risks associated with mineral exploration; fluctuations in commodity prices; title matters; and the additional risks identified in the annual information form of the Company or other reports and filings with the TSXV and applicable Canadian securities regulators. 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, except as required by applicable securities laws. Investors are cautioned against attributing undue certainty to forward-looking statements.

本新聞稿中所述的信息可能涉及適用證券法下的前瞻性陳述。前瞻性陳述是指與未來事件相關的聲明,而非過去事件。在此背景下,前瞻性陳述通常涉及預期的未來業務和財務表現,通常包含諸如「預期」、「相信」、「計劃」、「估計」、「期望」和「打算」等字眼,以及表示某項行爲或事件「可能」、「或許」、「能夠」、「應該」或「將」採取或發生的聲明,包括涉及礦物質潛在數量和/或品位、礦化區的潛在規模和擴展、擬定的勘探和開發計劃的時間安排或其他類似表述。除包含在此處的歷史事實陳述外,所有陳述均爲前瞻性陳述,包括但不限於有關收益使用的聲明。由於其性質,前瞻性陳述涉及已知和未知的風險、不確定性及其他可能導致我們的實際結果、表現或成就,或其他未來事件,與任何前瞻性陳述所表達或暗示的未來結果、表現或成就有重大差異的因素。這些因素包括但不限於以下風險:對額外融資的需求;與礦物勘探相關的操作風險;商品價格波動;所有權問題;以及在公司年度信息表或與TSXV及適用的加拿大證券監管機構的其他報告和文件中確定的其他風險。前瞻性陳述是基於管理層在做出聲明時的信念、估計和意見而作出,並且公司沒有義務在這些信念、估計和意見或其他情況發生變化時更新前瞻性陳述,除非適用的證券法要求。投資者應謹慎對待前瞻性陳述,不應過度確定其準確性。

Photos accompanying this announcement are available at:

隨此公告發佈的照片可在以下位置獲取:


声明:本內容僅用作提供資訊及教育之目的,不構成對任何特定投資或投資策略的推薦或認可。 更多信息
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