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Kalo Discovers New Epithermal Gold and Copper Mineralization at Vatu Aurum Gold Project, Fiji

Kalo Discovers New Epithermal Gold and Copper Mineralization at Vatu Aurum Gold Project, Fiji

Kalo 在斐濟 Vatu Aurum Gold 項目發現了新的超熱液金和銅礦化區
Accesswire ·  2023/09/27 21:20

Release Highlights:

發佈亮點:

  • Drilling at Drudrusavu has discovered a new epithermal vein system two kilometers east of the Qiriyaga Hill and Vuinubu Ridge Gold Deposits clearly associated with a prominent CSAMT high resistivity anomaly.
  • Drudrusavu mineralization is associated with at least two stages of epithermal mineralization, characterized by the presence of quartz sulfide veinlets and hydrothermal alteration, that have been documented over three intervals totaling 87.1 meters in KGD-2023-08 and 65.0 meters in KDG-2023-09.
  • Drilling at Mouta Prospect intersected two styles of mineralization primarily consisting of a broad zone of multi-directional epithermal sulfide veinlets consisting of zinc sulfides including sphalerite and marmatite, pyrite, and minor chalcopyrite with some caldera margin related shear-style mineralization.
  • 在Drudrusavu鑽探發現了一個新的淺成熱液脈系,位於齊裡亞加山和Vuinubu山脊以東兩公里處,明顯與CSAMT高電阻率異常有關。
  • Drudrusavu礦化與至少兩個以石英硫化物細脈和熱液蝕變為特徵的淺成熱液礦化有關,KGD-2023-08和KDG-2023-09記錄了三個總計87.1米和65.0米的淺成熱液礦化。
  • 在Mouta Prospects鑽探發現兩種類型的礦化,主要包括由閃鋅礦和鐵閃鋅礦等鋅硫化物、黃鐵礦和少量黃銅礦組成的寬闊的多向淺成低溫硫化物細脈,以及一些與破火山口邊緣有關的剪切式礦化。

VANCOUVER, BC / ACCESSWIRE / September 27, 2023 / KALO GOLD CORP. ("Kalo", "Kalo Gold" or the "Company") is pleased to provide an update on the exploration program at Vatu Aurum Gold Project ("Vatu Aurum" or the "Project"), Republic of Fiji. Kalo has completed four diamond drill holes in the 2023 exploration program: two at Drudrusavu ("Drudrusavu") located within the Qiriyaga Hill Prospect ("Qiriyaga") and two at Mouta Prospect ("Mouta") for a total of 432.0 meters ("m").

溫哥華,BC/ACCESSWIRE/2023年9月27日/Kalo Gold Corp.(“Kalo“,”Kalo Gold““或”公司“)很高興提供瓦圖奧魯姆金礦專案勘探計劃的最新情況(”瓦圖金“或”專案在2023年的勘探計劃中,卡洛已經完成了四個鑽石鑽孔:兩個在Drudrusavu(德魯薩瓦“)位於奇裡亞加山展望內(”奇裡亞加“)和兩個Mouta Prospects(”穆塔“),共432.0米(”M“)。

Mr. Terry L Tucker, P.Geo, President and CEO of Kalo Gold, commented "The two drill holes at Drudrusavu successfully confirmed the Controlled-Source Audio-frequency Magnetotellurics ("CSAMT") geophysical survey has identified zones of hydrothermal alteration and silicification. Both holes drilled had between 65 and 87 m of silicification and hydrothermal alteration and that included one interval that returned 4 meters averaging 1.23 g/t Au and 1 metre averaging 4.17 g/t Au. Given the shallow level of erosion that has been interpreted this indicates there is excellent potential for mineralization at depth at Drudrusavu. The positive correlation between the CSAMT and the drilling at Drudrusavu will give us the confidence to expand exploration at Qiriyaga. Previous drill results at Qiriyaga intersected thick, near-surface, high-grade gold mineralization, particularly drill hole KCD-17 that returned 8.75 metres at 36.02 g/t Au (61.25 to 70 m) and 10 m at 27.18 g/t Au (76-86 m) including 120 g/t Au between 81 to 82 m."

卡洛黃金首席執行官兼P.Geo總裁特裡·L·塔克先生評論道德魯魯薩武的兩個鑽孔成功地證實了可控源音頻大地電磁(“CSAMT“)地球物理測量已經確定了熱液蝕變和矽化帶。兩個鑽孔的矽化作用和熱液蝕變深度都在65到87米之間,其中包括一段返回層。4米平均1.23克/噸Au和1米平均4.17克/噸Au。考慮到已經解釋的淺部侵蝕程度,這表明在Drudrusavu有很好的深部礦化潛力。CSAMT與Drudrusavu鑽探之間的正相關性將使我們有信心擴大在齊裡亞加的勘探。之前在奇裡亞加的鑽探結果涉及厚的、近地表的高品位金礦化,特別是KCD-17鑽孔,返回8.75米,Au 36.02 g/t(61.25至70 m)和10米27.18 g/t Au(76-86 m),包括81至82 m之間的120 g/t Au。

Drudrusavu

德魯薩瓦

Two holes, KGD-2023-08 (232.50m) and KGD-2023-09 (169.50m) were drilled at Drudrusavu which is located 2 km east of Qiriyaga Hill and Vuinubu Ridge Gold Deposits. The drainage through Drudrusavu contained a "very strong gold anomaly" with gold in the stream sediment samples returning up to 580 parts per billion ("ppb") gold. Drudrusavu was originally defined by a 750 m long multi element soil and rock geochemical anomaly that was subsequently drilled in 1986 by Placer Dome. Drill holes KGD-2023-08 and KGD-2023-09 successfully tested the down dip extent of mineralized outcrop on Drudrusavu Creek, the soil geochemical anomaly, historical drilling and a prominent resistivity anomaly defined by a recently completed CSAMT survey (Target 5 in the previous release). The resistivity anomaly is believed to correspond to a ring fault around the edge of a caldera, a potential fertile corridor for precious metals mineralization (Figures 1 and 2).

在奇裡亞加山和維努布山脊金礦以東2公里處的Drudrusavu鑽了兩個孔,KGD-2023-08(232.50米)和KGD-2023-09(169.50米)。通過Drudrusavu的排水含有“非常強烈的金異常”,水系沉積物樣品中的金返回高達百萬分之580的金。Drudrusavu最初是由750米長的多元素土壤和岩石地球化學異常定義的,隨後於1986年由Placer Dome鑽探。KGD-2023-08和KGD-2023-09鑽孔成功地測試了Drudrusavu Creek礦化露頭的向下傾斜程度、土壤地球化學異常、歷史鑽探以及最近完成的CSAMT測量(上一次發佈的Target 5)確定的顯著電阻率異常。電阻率異常被認為對應於火山口邊緣的環狀斷層,火山口是貴金屬成礦的潛在富饒走廊(圖1和圖2)。

KGD-2023-08 intersected three mineralized zones from 50.4 to 85.5m, 115.5 to 157.5m and 206.1 to 216.1m composed of millimetre wide quartz veinlets with anhedral and open-space (comb) textures hosted in silica-chlorite altered polymictic breccia and dacite. Gold mineralization was intersected over a 4m zone averaging 1.23 grams per tonne ("g/t") gold, including a meter sample grading 4.17 g/t gold (see Table 1 and Photos 1 to 4).

KGD-2023-08在50.4-85.5米、115.5-157.5米和206.1-216.1m三個礦化帶相交,由毫米寬的石英細脈組成,無面體和開闊(梳狀)結構賦存於硅綠泥石蝕變多晶角礫巖和英安巖中。金礦化在一個4米區域,平均為每噸1.23克黃金,包括分級為4.17克/噸黃金的一米樣品(參見表1和照片1至4)。

KGD-2023-09 was drilled 100m to the southeast of KGD-2023-09 along the same CSAMT resistivity anomaly. It intersected three mineralized zones from 41.2 to 59.8m, 72.2 to 105.0m and 114.9 to 128.4m consisting of mm-wide quartz veinlets with comb texture associated with fine pyrite and chalcopyrite hosted in the same rock and alteration suite as KGD-2023-09.

KGD-2023-09在KGD-2023-09東南方向100米處,沿著相同的CSAMT電阻率異常鑽井。它橫跨41.2m-59.8m、72.2m-105.0m和114.9-128.4m三個礦化帶,由毫米寬的石英細脈組成,與細粒黃鐵礦和黃銅礦共生,賦存於與KGD2023-09相同的岩石和蝕變套中。

Table 1: Drudrusavu Drill Results
表1:Drudrusavu演習結果

The gold mineralization at Drudrusavu as shown in these two drill holes is associated with at least two stages of quartz veinlets.

這兩個鑽孔所顯示的Drudrusavu金礦與至少兩個階段的石英細脈有關。

  • Early-stage quartz veinlets and breccia filling with anhedral texture and a homogeneous appearance and an absence of banding, open-space, or similar features. This type of quartz generally infills the space between clasts of brecciated dacite. No other sulfides except pyrite have been documented with it.
  • A later-stage event with quartz veinlets-pyrite-chalcopyrite (centerline), was observed to cut the early quartz and is characterized by a cockscomb, open-space texture.
  • 早期的石英細脈和角礫巖充填,具有無面體結構和均勻的外觀,沒有帶狀、空曠或類似的特徵。這種類型的石英通常充填在角礫狀英安巖碎屑之間的空間。除了黃鐵礦以外,沒有其他硫化物被記錄在案。
  • 觀察到了一個以石英細脈-黃鐵礦-黃銅礦(中心線)為中心的後期事件,切割了早期石英,具有雞冠狀、開闊空間結構的特徵。

The relatively shallow oxidation level (~10m) at Drudrusavu suggests that the mineralization in the area will generally be primary. The results of the Drudrusavu drilling in addition to confirming gold mineralization in that area has extended the extent of the Qiriyaga Prospect a total of 2 km. The mineralization remains open along strike to the northeast and southeast and importantly at depth and correlates well with the CSAMT resistivity anomaly 5 as illustrated in Figure 3.

Drudrusavu的氧化程度相對較淺(~10m),表明該地區的礦化總體上將是原生的。Drudrusavu鑽探的結果除了證實該地區的金礦成礦作用外,還將齊裡亞加勘查範圍擴大了2公里。礦化沿走向向東北和東南方向保持開放,重要的是在深部,與CSAMT電阻率異常5有很好的相關性,如圖3所示。

Mouta Prospect

穆塔前景展望

Mouta Prospect ("Mouta") is located approximately 9 km northwest of Qiriyaga Hill Prospect on the outer edge of the Mouta Caldera. Two holes, KMD-2023-01 (151.5m) and KMD-2023-02 (280.5m) were drilled at Mouta to test a 330m long NE-trending soil anomaly characterized by coincident Au-Ag-As-Sb-Hg-Cu-Pb-Zn and a strong Induced Polarization ("IP") signature (see Figure 4).

Mouta Prospects(“Mouta”)位於Mouta火山口外邊緣的齊裡亞加山展望西北約9公里處。在Mouta鑽了兩個洞,KMD-2023-01(151.5米)和KMD-2023-02(280.5米),以測試330米長的NE向土壤異常,其特徵是Au-Ag-As-Sb-Hg-Cu-PbZn和強烈的激發極化(IP)特徵(見圖4)。

Two styles of mineralization were intersected, the first is the shear-style mineralized zone and the second is the broad zone of multi-directional epithermal sulfide veinlets consisting of zinc sulfides including sphalerite and marmatite, pyrite, and minor chalcopyrite. The mineralization is interpreted to be related to shallowly eroded phreatomagmatic eruption setting like the other Prospects on the Property.

兩種礦化類型交匯在一起,一種是剪切式礦化帶,另一種是由閃鋅礦、鐵閃鋅礦、黃鐵礦和少量黃銅礦等鋅硫化物組成的多向淺成熱液硫化物細脈的寬闊地帶。該礦化被解釋為與該礦體上的其他遠景一樣,與淺層侵蝕的雲母巖漿噴發環境有關。

KMD-2023-01 intersected the shear style mineralization from 31.0 to 51.0m hosted in a dark gray dacite breccia. It is gougy and strongly silicified in some sections with pyrite, chalcopyrite, and zinc sulfides (marmatite and sphalerite) up to 10% volume occurring as veinlets and disseminations. This zone is the downdip expression of the mineralized outcrop observed at the surface.

KMD-2023-0131.0~51.0m的剪切式礦化交匯於暗灰色英安巖角礫巖中。它呈泥狀,在某些部分強烈矽化,黃鐵礦、黃銅礦和硫化鋅(鐵閃鋅礦和閃鋅礦)體積高達10%,以細脈和散佈的形式出現。該帶是在地表觀察到的礦化露頭向下的表現。

The second style of mineralization was intersected from 51.0 to 69.0m in an intensely clay altered, felsic dacite breccia. The frequency of these veinlets is generally 5 to 10 per m and total sulfides are estimated between 5% to 7% volume. This zone was disrupted by an 8.40m, barren dark grey colored andesite dike from 68.2 to 76.6m but continued again until 94.0m. Mineralization tapered off from 94.0m downwards until a barren dacite flow (country rock) was hit at 117.80m.

第二類礦化從51.0米至69.0米,在強烈的黏土蝕變英安巖角礫巖中相交。這些小靜脈的頻率一般為每米5到10個,總硫化物的體積估計在5%到7%之間。這一地帶從68.2米到76.6米被一條8.40米、貧瘠的深灰色安山石堤壩打破,但再次延續到94.0米。礦化從94.0米向下逐漸減少,直到在117.80米處擊中了一條貧瘠的英安巖流(圍巖)。

KMD-2023-02 intersected the shear style mineralization from 30.55 to 45.30m within a highly oxidized zone that extends down to a depth of 59.40m. It intersected several 2m copper-bearing zones grading between 0.27% - 0.39% Cu with up to 3.56% Zn.

KMD-2023-02從30.55米至45.30米的剪切式礦化在向下延伸至59.40米的高度氧化帶內相交。它與幾個含銅品位在0.27%-0.39%之間的2M含銅帶相交,鋅品位可達3.56%。

The second style of mineralization was intersected from 129.5 to 178.0m. This zone is hosted within a silica - clay - chlorite altered dacite breccia from 129.50 m to 151.0m, and intense clay alteration from 151.0 to 178.0m. The sulfides identified within this zone are pyrite, zinc sulfides, and chalcopyrite and estimated to be up to 10%. KMD-2023-02 is mineralized from 178.0 m down to the end of hole at 280.5 m, but only pyrite was identified occurring both as fracture filling and disseminations in an intensely clay-altered dacite breccia. It returned 4 m averaging 0.59% from 167-171m.

第二類礦化相交於129.5~178.0m之間。該帶賦存於129.50~151.0米的硅黏土綠泥質蝕變英安巖角礫巖和151.0~178.0米的強烈黏土蝕變角礫巖中。在該帶內發現的硫化物有黃鐵礦、硫化鋅和黃銅礦,估計含量高達10%。KMD-2023-02在178.0米以下至280.5米處成礦,但在強烈黏土蝕變英安巖角礫巖中只發現黃鐵礦作為裂縫充填和擴散。它的回報率為400萬,平均為0.59%,從167-1.71億美元。

Table 2: Mouta Drill Results
表2:Mouta鑽探結果

Mouta Prospect - Surface Channel Sample Results

Mouta Prospects-地表通道採樣結果

Surface mapping has identified zones of silica, silica-clay, and clay alteration and the host rock of gold mineralization is a clay altered pumiceous dacite breccia. Argillic alteration can be intense locally and the main minerals are pyrite, sphalerite, chalcopyrite, chalcocite and barite. The presence of gold-silver-copper mineralization at Mouta Prospect, including: 6.2g/t Au, 645g/t Ag and 3.12% Cu from rock chip outcrop sampling and 3.06g/t Au, 819g/t Ag and 1.63% Cu from a stockpile grab sample have been received in addition to recently completed surface channel sampling of the mineralized outcrop. The table below summarizes the gold results from the channel sampling:

地表填圖已識別出硅質、硅質黏土和黏土蝕變帶,金礦化的賦礦岩石是黏土蝕變的浮石英安巖角礫巖。局部鋁石蝕變強烈,主要礦物有黃鐵礦、閃鋅礦、黃銅礦、輝銅礦和重晶石。木塔遠景中金-銀-銅礦化的存在,包括:6.2g/t金、645g/t銀和3.12%銅從露出地面的岩屑樣品和3.06克/噸金、819克/噸銀和1.63%銅除了最近完成的礦化露頭地表水道採樣外,還收到了從庫存中獲取的樣品。下表總結了通道採樣的GOLD結果:

Table 3: Mouta Surface Channel Sample Results
表3:Mouta Surface Channel採樣結果

The results of the work so far done in Mouta, including the two recently completed drill holes, has demonstrated that Mouta offers an opportunity for a gold or a gold-copper-zinc discovery. The Company will continue to evaluate the results for an effective follow up exploration program.

到目前為止在穆塔進行的工作的結果,包括最近完成的兩個鑽孔,表明穆塔提供了發現黃金或金-銅-鋅的機會。該公司將繼續評估結果,以便有效地實施後續勘探計劃。

Sampling, Analysis and QAQC

抽樣、分析和品質保證

The drill core was sampled at 1m intervals and cut into half with an electric core saw at the at the Company's exploration camp. The core samples were submitted to ALS Minerals laboratory in Brisbane, Australia ("ALS") for sample preparation and analysis. The gold was analyzed using Au-AA24 method (50g split). Multi-element analysis was also carried out using ME-ICP61m method. Kalo's Quality Control and Quality Assurance (QAQC) protocol for drill core samples includes: 1) field measurement of half core sample weights, 2) insertion of certified reference materials at 1 in 20 frequencies, 3) insertion of blank sample at 1 in 40 frequencies, and 3) insertion of duplicate core samples. ALS has internal QAQC protocols that include analysis and results monitoring for certified reference materials, blank samples, and duplicate core samples.

鑽芯每隔1米取樣一次,並在公司勘探營地用電動巖芯鋸切成兩半。岩心樣品被提交給澳大利亞布裡斯班的ALS Minerals實驗室(“ALS”)進行樣品準備和分析。金的分析採用Au-AA24法(50g Split)。採用ME-ICP61M法進行多元素分析。Kalo針對鑽探岩心樣品的質量控制和品質保證(QAQC)協定包括:1)現場測量半岩心樣品重量;2)以20個頻率中的1個頻率插入經認證的標準物質;3)以40個頻率中的1個頻率插入空白樣品;以及3)插入重複的岩心樣品。ALS有內部QAQC協定,包括對經認證的標準物質、空白樣品和複製的核心樣品的分析和結果監測。

ABOUT KALO GOLD CORP.

關於卡洛黃金公司。

Kalo Gold Corp, a gold exploration company, is focused on exploration for low sulphidation epithermal gold deposits of the Vatu Aurum Gold Project on the island of Vanua Levu (North Island) in the Republic of Fiji. Kalo holds a 100% interest in two Special Prospecting Licenses, covering 367 km2 that hosts a minimum of seven volcanic arc related calderas ranging between 1 to 10km in diameter in a geological setting that could be analogous to the alkaline related low sulphidation epithermal gold deposits of both the neighbouring Vatukoula Gold Mine and the Lion One Metals' Tuvatu Alkaline Gold Project. Historical exploration work concentrated on the Qiriyaga Hill and Vuinubu Ridge Gold Deposits and resulted in the identification of over fourteen priority epithermal gold exploration targets.

Kalo Gold Corp是一家黃金勘探公司,專注於斐濟共和國瓦努阿列武島(北島)Vatu Aurum金礦專案的低硫化低溫熱液金礦勘探。Kalo擁有兩個特殊勘探許可證的100%權益,覆蓋367公里2.該地區至少有7個與火山弧有關的火山口,直徑在1至10公里之間,其地質環境類似於鄰近的瓦圖庫拉金礦和Lion One Metals的Tuvatu鹼性金礦專案中與鹼性有關的低硫化低溫熱液金礦。歷史勘探工作集中在奇裡亞加山和維努布山脊金礦床上,確定了14個優先的淺成熱液金礦勘探目標。

Both Viti Levu, (South Island), and Vanua Levu are on the prolific Pacific "Ring of Fire", a trend that has produced numerous large deposits, including Porgera, Lihir and Grasberg and on Viti Levu, the exceptional Vatukoula Gold Mine. The Vatukoula Gold Mine has produced more than 7 million ounces of gold since 1937. The island of Viti Levu also hosts the fully permitted Tuvatu Alkaline Gold Project, where Lion One Metals is fast tracking a high-grade underground gold mining operation.

南島的Viti Levu和Vanua Levu都位於多產的太平洋“火環”上,這一趨勢已經產生了許多大型礦藏,包括Porgera、Lihir和Grasberg,以及特殊的Vatukoula金礦Viti Levu。自1937年以來,瓦圖庫拉金礦已經生產了700多萬盎司黃金。Viti Levu島還擁有完全許可的Tuvatu鹼性金礦專案,Lion One Metals正在快速追蹤一個高品位地下金礦開採業務。

Qualified Person

有資格的人

The technical disclosure in this news release has been approved by Terry L. Tucker, P.Geo. a Qualified Person as defined by National Instrument 43-101 of the Canadian Securities Administrators.

本新聞稿中的技術披露已得到Terry L.Tucker,P.Geo的批准。加拿大證券管理人的國家文書43-101所定義的合格人員。

On behalf of the Board of Directors of Kalo Gold Corp.

我謹代表Kalo Gold Corp.董事會發言。

Terry L. Tucker, P.Geo
President and Chief Executive Officer
and
Kevin Ma, CPA, CA
Executive Vice President, Capital Markets and Director

特裡·L·塔克,P.Geo
總裁與首席執行官

Kevin Ma,註冊會計師,加利福尼亞州
資本市場部和董事常務副總裁總裁

For more information, please write to info@kalogoldcorp.com.

欲瞭解更多資訊,請寫信至info@kalogoldcorp.com。

Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the Exchange) accepts responsibility for the adequacy or accuracy of this press release.

多倫多證券交易所創業板交易所及其監管服務提供商(該術語在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。

Forward Looking Statements Disclaimer

前瞻性聲明免責聲明

Certain statements in this release are forward-looking statements, which are statements that are not purely historical, including any statements regarding beliefs, plans, expectations, or intentions regarding the future. Forward looking statements in this news release include statements relating to the Company's proposed drilling timeline and the proposed expansion of the exploration program, and the Company's plans for future exploration on the Vatu Aurum Gold Project. Forward-looking statements are often identified by terms such as "will", "may", "should", "anticipate", "expects" and similar expressions. All statements included in this news release, other than statements of historical fact, are forward-looking statements that involve risks and uncertainties. There can be no assurance that such statements will prove to be accurate and actual results, and future events could differ materially from those anticipated in such statements. Important factors that could cause actual results to differ materially from the Company's expectations include quality and quantity of any mineral deposits that may be located, the Company's inability to obtain any necessary permits, consents or authorizations required for its activities, the Company's inability to raise the necessary capital to be fully able to implement its business strategies, and other risks and uncertainties disclosed in the Company's filing statement dated February 9, 2021 and latest interim Management Discussion and Analysis filed with certain securities commissions in Canada.

本新聞稿中的某些陳述是前瞻性陳述,這些陳述不是純粹的歷史性陳述,包括任何有關對未來的信念、計劃、預期或意圖的陳述。本新聞稿中的前瞻性陳述包括與公司擬議的鑽井時間表和擬議的勘探計劃擴大有關的陳述,以及公司未來在Vatu Aurum Gold的勘探計劃 專案。前瞻性陳述通常用“將”、“可能”、“應該”、“預期”、“預期”和類似的表達方式來識別。除歷史事實陳述外,本新聞稿中包含的所有陳述均為前瞻性陳述,涉及風險和不確定因素。不能保證這些陳述將被證明是準確和實際的結果,未來的事件可能與這些陳述中預期的大不相同。可能導致實際結果與公司預期大相徑庭的重要因素包括可能存在的任何礦藏的質量和數量、公司無法獲得其活動所需的任何必要許可、同意或授權、公司無法籌集必要的資本以充分實施其業務戰略,以及公司在2021年2月9日的申報聲明和最近提交給加拿大某些證券委員會的中期管理層討論和分析中披露的其他風險和不確定因素。

The reader is cautioned that assumptions used in the preparation of any forward-looking statements herein may prove to be incorrect. Events or circumstances may cause actual results to differ materially from those predicted, as a result of numerous known and unknown risks, uncertainties, and other factors, many of which are beyond the control of the Company. The reader is cautioned not to place undue reliance on any forward-looking information. Such information, although considered reasonable by management at the time of preparation, may prove to be incorrect, and actual results may differ materially from those anticipated. Forward-looking statements contained in this news release are expressly qualified by this cautionary statement. The forward-looking statements contained in this news release are made as of the date of this news release and the Company will update or revise publicly any of the included forward-looking statements as expressly required by Canadian securities law.

提醒讀者,在編制本文中的任何前瞻性陳述時使用的假設可能被證明是不正確的。由於許多已知和未知的風險、不確定性和其他因素,其中許多是公司無法控制的,事件或情況可能會導致實際結果與預測的結果大不相同。提醒讀者不要過度依賴任何前瞻性資訊。這些資訊雖然在準備時被管理層認為是合理的,但可能被證明是不正確的,實際結果可能與預期的大不相同。本新聞稿中包含的前瞻性陳述明確地受到本警示性聲明的限制。本新聞稿中包含的前瞻性陳述是截至本新聞稿發佈之日作出的,公司將按照加拿大證券法的明確要求更新或公開修改任何包含的前瞻性陳述。

Figure 1: Vatu Aurum Gold Project - 2023 drilling to date (blue circles) at Mouta and Qiriyaga Hill Prospects.
圖1:Vatu Aurum金礦專案-2023年迄今在穆塔山和奇裡亞加山的鑽探(藍圈)前景
Figure 2: Vatu Aurum Gold Project - 2023 drilling to date (blue circles) at Qiriyaga Hill Prospect.
圖2:Vatu Aurum金礦專案--到目前為止在奇裡亞加山勘探的2023年鑽探(藍圈)。
Figure 3: Qiriyiga Hill Prospect - CSAMT 1D Inversion at 200 meters with six key target zones identified.
圖3:奇裡伊加山展望-CSAMT一維200米反演,確定了六個關鍵目標區。
Figure 4: Vatu Aurum Gold Project - 2023 drilling to date (blue circles) at Mouta Prospect.
圖4:Vatu Aurum金礦專案-2023年迄今在Mouta Prospects鑽探(藍色圓圈)。
Photo 1: KGD-2023-08: Intense quartz - pyrite infill from 53.0 to 54.0m. Assays returned 4m at 1.23 g/t Au from 53 to 57m with 1m at 4.17 g/t Au from 53 to 54m.
圖1:KGD-2023-08:從53.0米到54.0米的強烈石英-黃鐵礦充填。從53到57個月,化驗結果為1.23克/噸金,回收4個月;從53到54個月,以4.17克/噸金回收1個月。
Photo 2: KGD-2023-08: Close-up of the interval which returned 4.17 g/t Au from 53 to 54m. Note the abundant quartz veining with open-space texture.
圖2:KGD-2023-08:距離特寫,從53米返回4.17克/噸金至54米。注意豐富的石英脈和開放的空間結構。
Photo 3: KGD-2023-08: Banded, 5cm quartz-py-cpy veinlet; note the hydrothermal brecciation of the host rock. Assays returned 1m at 1.58% Cu and 21 g/t Ag from 74 to 75m.
圖3:KGD-2023-08:帶狀,5釐米厚的石英細脈;注意到主巖的熱液角礫巖。當銅含量為1.58%,銀含量為21g/t時,測定結果為1M,從74到75M。
Photo 4: KGD-2023-08: Close-up of the banded, 5cm qz-py-cpy veinlet at 74.45. Assays returned 1m at 1.54% Cu and 21 g/t Ag from 74 to 75m.
圖4:KGD-2023-08:74.45處的5釐米帶狀QZ-PY-CPY靜脈入口的特寫。當銅含量為1.54%,銀含量為21g/t時,測定結果為1M,從74到75M。

SOURCE: Kalo Gold Corp.

資料來源:卡洛黃金公司


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