Vancouver, British Columbia--(Newsfile Corp. - February 22, 2024) - Cabral Gold Inc. (TSXV: CBR) (OTC PINK: CBGZF) ("Cabral" or the "Company") is pleased to announce assay results from an additional 13 RC holes testing near-surface oxide material at the Central gold deposit, and nine shallow auger holes from the MG gold deposit, Cuiú Cuiú gold district in northern Brazil. These holes are part of a drill program designed to expand and upgrade the oxide resources at both the Central and MG gold deposits.
Highlights
- RC390 returned 23m @ 1.0 g/t gold from 5m depth in mineralized basement saprolite
- RC391 returned 13m @ 1.4 g/t gold from 51m depth in mineralized basement saprolite. The hole also intersected 4m @ 1.2 g/t gold from 40m depth
- Eleven of the 13 RC holes returned gold values within the weathered material at Central which comprises overlying sediments that form a blanket that is underlain by weathered granitic material or saprolite. Other notable drill results include 3m @ 2.5 g/t gold from 25m depth and 5m @ 1.9 g/t gold from 61m depth in RC387
- Eight of the nine shallow auger holes drilled at the MG gold deposit returned gold values well above the cut-off grade of 0.14 g/t gold, with TR665 returning 19m @ 1.3 g/t gold from surface including 2m @ 8.0 g/t gold
Alan Carter, Cabral's President and CEO commented, "These additional results from the RC drilling at Central and the auger drilling at MG build on earlier drill results that show the widespread presence of gold in the near-surface blanket sedimentary material and the underlying weathered basement rocks or saprolite at concentrations well above the cut-off grade of 0.14 g/t gold which was applied to the most recent resource estimate of July 2022 for this oxide material."
Central RC Drill Results
The Central gold deposit is one of the two main gold deposits identified to date at Cuiú Cuiú. As with the nearby MG gold deposit, the upper portion of the Central gold deposit is extensively weathered resulting in a vertical profile of highly weathered basement saprolite averaging approximately 60m. The weathered mineralized basement saprolite is overlain by sediments which form a blanket. The blanket material contains gold and is derived from the chemical and physical weathering of the underlying saprolite basement gold mineralization.
Whilst the bulk of the gold resources at Central are contained within the underlying primary (un-weathered) basement material (see the NI 43-101 report dated effective July 31, 2022), the overlying oxide material currently contains Indicated Resources of 3.49Mt @ 0.6 g/t gold (65,400oz) and Inferred Resources of 3.36Mt @ 0.4 g/t gold (44,800oz). A significant amount of higher-grade material (greater than 1.75g/t gold) is contained within these resources and the current drill program at Central and MG is designed to expand and delimit these resources within the near-surface saprolite and blanket material.
Cut-off grades of 0.14 g/t gold and 0.26 g/t gold were used for the 2022 open pit resource estimate for blanket/saprolite and fresh-rock mineralization, respectively.
Holes RC386 to RC398 were all drilled within the overall outline of the oxide resource at Central to a maximum depth of 90m (Figure 1).
Figure 1: Map showing Central gold deposit with limits to oxide blanket and underlying mineralized zones in weathered basement saprolite, existing RC and diamond-drill holes and new drill holes, RC386 to RC398 with results. Previous RC holes are also shown with significant results. Terms; g/t = grams / tonne, m = metres
Section N21095
RC390 was designed to test the north eastern part of this section. Drill results from adjacent sections at Central, for example RC384 which was drilled on section N21198, 100m further north and returned 23m @ 0.9 g/t gold, suggested the presence of gold mineralization in the overlying blanket sediments and primary saprolite material in this area (see press release dated January 11, 2024).
RC390 returned 23m @ 1.0 g/t gold from 5m depth in saprolite, and encountered 3m @ 0.6 g/t gold from surface in the unconformably overlying blanket. This saprolite intercept is interpreted to be the same mineralized zone that was intersected by hole RC384 drilled 100m further north.
Figure 2: Section N21095 through the Central gold deposit showing the near surface gold-in-oxide saprolite layer and overlying blanket sediments assay results for drill hole RC390 and previous RC drill holes. Terms; g/t = grams / tonne, m = metres, ppm = parts per million or grams / tonne
Section N20845
Hole RC391 was drilled on section N20845 in the southern part of the Central gold deposit. Previous drilling on this section returned remarkably consistent gold values in the overlying blanket soils and sediments of 0.6 to 0.7 g/t gold, for example 18.3m @ 0.7 g/t gold from surface in DDH265 (Figures 1 and 3, Table 1).
RC391 returned 13m @ 1.4 g/t gold from 51m depth. This is interpreted to be the same mineralized zone that was intersected by hole DDH267 which returned 12.8m @ 1.0 g/t gold within unweathered primary basement granitic rocks, and indicates the presence of gold values of +1 g/t in saprolite on this section. These grades are significantly better than grades obtained from other holes that tested the saprolite on this section.
There was no material recovered by drilling in the top 14m of the hole but that interval is expected to be mineralized based on results from adjacent holes, i.e. DDH265 and DDH266 which returned 18.3m @ 0.7 g/t gold and 12m @ 0.7 g/t gold from surface, respectively.
Figure 3: Section N20845 through the Central gold deposit showing the near surface gold-in-oxide saprolite layer and overlying blanket sediments assay results for RC drill hole RC391 and previous diamond drill holes. Terms; g/t = grams / tonne, m = metres, ppm = parts per million or grams / tonne
Drill Hole | Weathering | | | From | To | Width | Grade |
# | | | | m | m | m | g/t gold |
RC0386 | Blanket | | | 0.0 | 3.0 | 3.0 | 0.72 |
| | EOH | 49.0 | | | | |
RC03871 | Blanket | | | 0.0 | 2.0 | 2.0 | 0.46 |
| Saprolite | | | 25.0 | 28.0 | 3.0 | 2.51 |
| Fresh Rock | | | 61.0 | 66.0 | 5.0 | 1.92 |
| | EOH | 66.0 | | | | |
RC0388 | Blanket | | | | | | N.S.V. |
| | EOH | 69.0 | | | | |
RC0389 | Saprolite | | | 61.0 | 69.0 | 8.0 | 0.68 |
| | EOH | 76.0 | | | | |
RC0390 | Blanket | | | 0.0 | 3.0 | 3.0 | 0.61 |
| Saprolite | | | 5.0 | 28.0 | 23.0 | 1.05 |
| | EOH | 54.0 | | | | |
RC03912 | Saprolite | | | 25.0 | 27.0 | 2.0 | 0.52 |
| | | | 40.0 | 44.0 | 4.0 | 1.18 |
| | | | 51.0 | 64.0 | 13.0 | 1.37 |
| | EOH | 74.0 | | | | |
RC03923 | Blanket | | | 0.0 | 4.0 | 4.0 | 0.71 |
| | EOH | 60.0 | | | | |
RC0393 | Blanket | | | | | 0.0 | N.S.V. |
| | EOH | 90.0 | | | | |
RC0394 | Saprolite | | | 17.0 | 19.0 | 2.0 | 2.85 |
| | | | 41.0 | 47.0 | 6.0 | 0.44 |
| | | | 70.0 | 73.0 | 3.0 | 1.19 |
| | EOH | 77.0 | | | | |
RC0395 | Blanket | | | 0.0 | 5.0 | 5.0 | 0.27 |
| | EOH | 70.0 | | | | |
RC0396 | Saprolite | | | 8.0 | 10.0 | 2.0 | 2.13 |
| | EOH | 86.0 | | | | |
RC0397 | Blanket | | | 0.0 | 6.0 | 6.0 | 0.57 |
| | EOH | 66.0 | | | | |
RC0398 | Saprolite | | | 10.0 | 12.0 | 2.0 | 1.08 |
| | EOH | 55.0 | | | | |
Table 1: Drill results from near surface Central gold-in-oxide blanket / saprolite zone regarding holes RC386 to RC398.
1 No recovery in RC387 from 2-4m, 5-9m, 11-12m and 13-14m.
2 No recovery in RC391 from 0-14m.
3 No recovery in RC392 from 4-22m. Terms; g/t = grams / tonne, m = metres, N.S.V. = no significant values
MG Auger Drill Results
The MG gold deposit is the second of the two main gold deposits that have been identified to date at Cuiú Cuiú. As with the nearby Central gold deposit, the upper portion of the MG gold deposit is extensively weathered resulting in a vertical profile of approximately 60m of highly weathered basement saprolite. The weathered mineralized basement saprolite is overlain by mud, soil and colluvium material which forms a blanket. All of the blanket material contains gold and is derived from the chemical and physical weathering of the underlying saprolite basement gold mineralization.
Whilst the bulk of the gold resources at MG are contained within the underlying primary (unweathered) basement material (see the NI 43-101 report dated effective July 31, 2022), the overlying oxide material currently contains Indicated Resources of 5.78Mt @ 0.5 g/t for 88,300oz, and Inferred Resources of 1.19Mt @ 0.3 g/t for 12,300oz. A significant amount of higher-grade material (greater than 1.75g/t gold) is contained within these resources and the recent RC and auger drill program at MG is designed to expand these resources within the near-surface saprolite and blanket material.
Recent RC drill results from MG reported as part of the current program have returned some very significant results in the oxidized near-surface blanket sediments and underlying saprolite including hole RC343 which returned 27m @ 1.9 g/t gold from surface, RC342 which returned 28m @ 1.8 g/t gold from surface, RC375 which returned 20m @ 1.6 g/t gold from surface including 9m @ 1.7 g/t gold and RC376 which returned 15m @ 1.8 g/t gold from 5m depth (see press releases dated October 12, 2023 and November 29, 2023).
Nine auger holes are reported here with results from TR657 to TR665 (See Table 2 and Figures 4 and 5).
Figure 4. Map showing MG gold deposit with limits to oxide blanket and underlying mineralized zones in weathered basement saprolite with results from auger holes TR658 to TR665. Terms; g/t = grams / tonne, m = metres
Section 553500
Auger hole TR665 was drilled on section 553500 (Figures 4 and 5, Table 2). Previous diamond and RC drilling on this section had outlined an area of consistent mineralization in the blanket sediments in the order of 0.5 g/t gold, for example, RC315 returned 46m @ 0.5 g/t gold and RC134 which returned 26m @ 0.5 g/t gold).
TR665 was drilled further to the north-east and returned significantly higher gold values than expected including 19m @ 1.3 g/t gold from surface including 2m @ 8.0 g/t gold from 10m depth. The hole ended in mineralization. These results suggest the presence of a zone of higher-grade gold mineralization than previously anticipated on this section in the near-surface blanket sediments.
Figure 5: Section 553500 through the MG gold deposit showing the near surface gold-in-oxide saprolite layer and assay results for recent auger hole TR665, as well as results for previous RC and diamond drill holes. Terms; g/t = grams / tonne, m = metres, ppm = parts per million or grams / tonne
Drill Hole | Weathering | | | From | To | Width | Grade |
# | | | | m | m | m | g/t gold |
TR0657 | Blanket/Saprolite | | | | | 0.0 | N.S.V. |
| | EOH | 20.0 | | | | |
TR0658 | Blanket/Saprolite | | | 8.0 | 16.0 | 8.0 | 0.49 |
| | EOH | 17.0 | | | | |
TR0659 | Blanket/Saprolite | | | 2.0 | 18.0 | 16.0 | 0.37 |
| | EOH | 18.0 | | | | |
TR0660 | Blanket/Saprolite | | | 3.0 | 19.0 | 16.0 | 0.36 |
| | EOH | 19.0 | | | | |
TR0661 | Blanket/Saprolite | | | 8.0 | 16.0 | 8.0 | 0.32 |
| | EOH | 20.0 | | | | |
TR0662 | Blanket/Saprolite | | | 8.0 | 18.0 | 10.0 | 0.49 |
| | EOH | 18.0 | | | | |
TR0663 | Blanket/Saprolite | | | 0.0 | 20.0 | 20.0 | 0.34 |
| | EOH | 20.0 | | | | |
TR0664 | Blanket/Saprolite | | | 0.0 | 20.0 | 20.0 | 0.31 |
| | EOH | 20.0 | | | | |
TR0665 | Blanket/Saprolite | | | 0.0 | 19.0 | 19.0 | 1.26 |
| | | incl | 10.0 | 12.0 | 2.0 | 7.95 |
| | EOH | 19.0 | | | | |
Table 2: Auger drill results from near surface MG gold-in-oxide blanket / saprolite zone regarding holes TR658 to TR665.
Terms; g/t = grams / tonne, m = metres, N.S.V. = no significant values
About Cabral Gold Inc.
The Company is a junior resource company engaged in the identification, exploration and development of mineral properties, with a primary focus on gold properties located in Brazil. The Company has a 100% interest in the Cuiú Cuiú gold district located in the Tapajós Region, within the state of Pará in northern Brazil. Two main gold deposits have so far been defined at the Cuiú Cuiú project which contains National Instrument 43-101 compliant Indicated resources of 21.6Mt @ 0.87 g/t gold (604,000 oz) and Inferred resources of 19.8Mt @ 0.84 g/t gold (534,500 oz) as per the 43-101 technical report dated October 12, 2022.
The Tapajós Gold Province is the site of the largest gold rush in Brazil's history which according to the ANM (Agência Nacional de Mineração or National Mining Agency of Brazil) produced an estimated 30 to 50 million ounces of placer gold between 1978 and 1995. Cuiú Cuiú was the largest area of placer workings in the Tapajós and produced an estimated 2Moz of placer gold historically.
FOR FURTHER INFORMATION PLEASE CONTACT:
"Alan Carter"
President and Chief Executive Officer
Cabral Gold Inc.
Tel: 604.676.5660
Guillermo Hughes, MAusIMM and FAIG., a consultant to the Company as well as a Qualified Person as defined by National Instrument 43-101, supervised the preparation of the technical information in this news release.
Neither the TSX Venture Exchange nor its Regulation Services Provider (as such term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of this release.
Forward-looking Statements
This news release contains certain forward-looking information and forward-looking statements within the meaning of applicable securities legislation (collectively "forward-looking statements"). The use of the words "will", "expected" and similar expressions are intended to identify forward-looking statements. These statements involve known and unknown risks, uncertainties and other factors that may cause actual results or events to differ materially from those anticipated in such forward-looking statements. Such forward-looking statements should not be unduly relied upon. The Company believes the expectations reflected in those forward-looking statements are reasonable, but no assurance can be given that these expectations will prove to be correct.
Notes
Gold analysis has been conducted by SGS method FAA505 (fire assay of 50g charge), with higher grade samples checked by FAA525. Analytical quality is monitored by certified references and blanks. Until dispatch, samples are stored under the supervision the Company's exploration office. The samples are couriered to the assay laboratory using a commercial contractor. Pulps are returned to the Company and archived. Drill holes results are quoted as down-hole length weighted intersections.
不列顛哥倫比亞省溫哥華--(Newsfile Corp.-2024 年 2 月 22 日)- Cabral Gold Inc.(多倫多證券交易所股票代碼:CBR)(場外交易代碼:CBGZF) (“卡布拉爾” 或 “公司“)很高興地宣佈在中央金礦牀上測試近地表氧化物質的另外13個RC孔以及來自巴西北部Cuiué Cuiu'金礦區MG金礦牀的9個淺螺旋孔的化驗結果。這些鑽孔是鑽探計劃的一部分,該計劃旨在擴大和升級Central和MG金礦牀的氧化物資源。
亮點
- RC390 回來了 23m @ 1.0 g/t 黃金 從 5 米深的礦化基底腐爛巖中
- RC391 回來了 13m @ 1.4 g/t 黃金 從 51 米深的礦化基底腐爛巖中產生。洞也相交了 4m @ 1.2 g/t 黃金 從 40 米深度開始
- 在13個RC孔中,有11個在中部的風化物質中返回了金值,這些物質包括上覆的沉積物,形成了一層被風化的花崗岩材料或腐爛巖覆蓋的覆蓋層。其他值得注意的鑽探結果包括 3m @ 2.5 g/t 黃金 從 25 米深度開始 5m @ 1.9 g/t 黃金 在 RC387 中,從 61 米的深度出發
- 在 MG 金礦牀鑽探的九個淺螺旋鑽孔中,有八個返回的黃金價值遠高於 0.14 g/t 黃金的臨界品位,TR665 又回來了 19 米 @ 1.3 克/噸黃金 來自表面,包括 2m @ 8.0 g/t 金幣
卡布拉爾總裁兼首席執行官艾倫·卡特評論說:“Central的RC鑽探和MG的螺旋鑽探的這些額外結果建立在先前的鑽探結果基礎上,這些結果表明,近地表層沉積物和底層風化的基底岩石或腐殖巖中廣泛存在金,其濃度遠高於0.14克/噸金的臨界品位,該金的臨界品位是應用於2022年7月這種氧化物材料的最新資源估算值的。”
中央遙控鑽探結果
中央金礦是迄今爲止在庫伊烏庫伊確定的兩個主要金礦牀之一。與附近的MG金礦牀一樣,中央金礦牀的上部被廣泛風化,形成了高度風化的基底腐殖巖的垂直剖面,平均約爲60米。風化的礦化基底腐爛巖被沉積物覆蓋,形成覆蓋層。這種覆蓋層材料含有金,源自底層腐爛岩基底金礦化的化學和物理風化。
雖然中環的大部分黃金資源都包含在基礎的初級(未風化)基底材料中(參見2022年7月31日生效的NI 43-101報告),但上覆的氧化物材料目前含有3.49萬噸(0.6克/噸黃金(65,400盎司)的指示資源和3.36萬噸的0.4克/噸黃金(44,800盎司)的推斷資源。這些資源中含有大量更高品位的材料(超過1.75g/t的黃金),目前在Central和MG的鑽探計劃旨在擴大和界定近地表腐殖巖和覆蓋材料中的這些資源。
2022年對毯狀/腐爛巖和新鮮岩石礦化的露天資源估算分別使用了0.14克/噸金和0.26克/噸金的臨界品位。
RC386 至 RC398 的孔都是在中央氧化物資源的總體輪廓內鑽探的,最大深度爲 90 米(圖 1)。
圖 1:地圖顯示了風化基底腐殖巖中氧化層和底層礦化帶極限的中央金礦牀、現有的 RC 和金剛石鑽孔以及新鑽孔(從 RC386 到 RC398)以及結果。之前的 RC 孔也顯示了顯著的結果。條款;g/t = 克/噸,m = 米
第 N21095 節
RC390 旨在測試該路段的東北部分。來自中部相鄰路段的鑽探結果,例如 RC384,它在向北 100 米處的 N21198 路段鑽探後返回 23m @ 0.9 g/t 黃金,表明該地區上覆的覆蓋層沉積物和初級腐生巖物質中存在金礦化(見2024年1月11日的新聞稿)。
RC390 回來了 23m @ 1.0 g/t 黃金 在 saprolite 的 5 米深處,在不適宜的覆蓋層中遇到了來自表面的 3m @ 0.6 g/t 的金。這個腐爛巖截距被解釋爲與向北 100 米處鑽出的 RC384 孔相交的礦化帶相同。
圖 2:穿過中央金礦牀的 N21095 截面顯示了 RC390 鑽孔和先前 RC 鑽孔的近地表氧化金腐爛岩層和覆蓋的覆蓋層沉積物的分析結果。術語;g/t = 克/噸,m = 米,ppm = 百萬分之一或克/噸
第 N20845 節
RC391 洞是在中央金礦牀南部的 N20845 區段鑽探的。例如,先前對該部分的鑽探表明,上覆的覆蓋層土壤和沉積物中的金值非常穩定,爲0.6至0.7 g/t的金 18.3 米 @ 0.7 克/噸黃金 從 DDH265 的表面開始(圖 1 和 3,表 1)。
RC391 回來了 13m @ 1.4 g/t 黃金 從 51 米深度開始。這被解釋爲與返回的 DDH267 孔相交的礦化帶相同 12.8 米 @ 1.0 克/噸黃金 在未經風化的初級基底花崗岩中,並表明該部分腐爛巖中的金值爲+1 g/t。這些等級明顯優於在本部分測試腐爛巖的其他孔洞中獲得的等級。
在鑽孔頂部 14m 處鑽探沒有回收任何材料,但根據相鄰鑽孔(即返回的 DDH265 和 DDH266)的結果,預計該間隔將進行礦化 18.3 米 @ 0.7 克/噸黃金 和 12m @ 0.7 g/t 黃金 分別從表面上看。
圖 3:穿過中央金礦牀的 N20845 截面顯示了 RC 鑽孔 RC391 和先前金剛石鑽孔的近地表氧化金腐爛岩層和覆蓋的覆蓋層沉積物的分析結果。術語;g/t = 克/噸,m = 米,ppm = 百萬分之一或克/噸
鑽孔 | 風化 | | | 來自 | 到 | 寬度 | 等級 |
# | | | | m | m | m | g/t 黃金 |
RC0386 | 毛毯 | | | 0.0 | 3.0 | 3.0 | 0.72 |
| | 哎喲 | 49.0 | | | | |
RC03871 | 毛毯 | | | 0.0 | 2.0 | 2.0 | 0.46 |
| Saprolite | | | 25.0 | 28.0 | 3.0 | 2.51 |
| 新鮮搖滾 | | | 61.0 | 66.0 | 5.0 | 1.92 |
| | 哎喲 | 66.0 | | | | |
RC0388 | 毛毯 | | | | | | N.S.V。 |
| | 哎喲 | 69.0 | | | | |
RC0389 | Saprolite | | | 61.0 | 69.0 | 8.0 | 0.68 |
| | 哎喲 | 76.0 | | | | |
RC0390 | 毛毯 | | | 0.0 | 3.0 | 3.0 | 0.61 |
| Saprolite | | | 5.0 | 28.0 | 23.0 | 1.05 |
| | 哎喲 | 54.0 | | | | |
RC03912 | Saprolite | | | 25.0 | 27.0 | 2.0 | 0.52 |
| | | | 40.0 | 44.0 | 4.0 | 1.18 |
| | | | 51.0 | 64.0 | 13.0 | 1.37 |
| | 哎喲 | 74.0 | | | | |
RC03923 | 毛毯 | | | 0.0 | 4.0 | 4.0 | 0.71 |
| | 哎喲 | 60.0 | | | | |
RC0393 | 毛毯 | | | | | 0.0 | N.S.V。 |
| | 哎喲 | 90.0 | | | | |
RC0394 | Saprolite | | | 17.0 | 19.0 | 2.0 | 2.85 |
| | | | 41.0 | 47.0 | 6.0 | 0.44 |
| | | | 70.0 | 73.0 | 3.0 | 1.19 |
| | 哎喲 | 77.0 | | | | |
RC0395 | 毛毯 | | | 0.0 | 5.0 | 5.0 | 0.27 |
| | 哎喲 | 70.0 | | | | |
RC0396 | Saprolite | | | 8.0 | 10.0 | 2.0 | 2.13 |
| | 哎喲 | 86.0 | | | | |
RC0397 | 毛毯 | | | 0.0 | 6.0 | 6.0 | 0.57 |
| | 哎喲 | 66.0 | | | | |
RC0398 | Saprolite | | | 10.0 | 12.0 | 2.0 | 1.08 |
| | 哎喲 | 55.0 | | | | |
表 1:關於 RC386 至 RC398 孔洞的近地表中央氧化金覆蓋層/腐蝕巖區域的鑽探結果。
1 RC387 無法從 2-4m、5-9m、11-12m 和 13-14m 恢復。
2 RC391 從 0-14m 沒有恢復。
3 RC392 無法從 4-22 米恢復。條款;g/t = 克/噸,m = 米,N.S.V. = 無有效值
MG 螺旋鑽機結果
MG金礦是迄今爲止在Cuiué Cuiuí發現的兩個主要金礦牀中的第二個。與附近的中央金礦牀一樣,MG金礦牀的上部被廣泛風化,形成了大約60m高度風化的基底腐殖巖的垂直剖面。風化的礦化基底腐爛巖被泥土、土壤和堆積物覆蓋,形成一層毯子。所有覆蓋材料都含有金,源自底層腐爛岩基底金礦化的化學和物理風化。
儘管MG的大部分黃金資源都包含在潛在的主要(未風化)基底材料中(見2022年7月31日生效的NI 43-101報告),但上覆的氧化物材料目前含有88,300盎司的578萬噸/0.5克/噸的指示資源,12,300盎司的推斷資源爲119萬噸(0.3克/噸)。這些資源中含有大量更高品位的材料(超過1.75g/t的黃金),MG最近的RC和螺旋鑽探計劃旨在將這些資源擴展到近地表腐殖巖和毯狀材料中。
作爲當前計劃的一部分,MG 最近報告的 RC 鑽探結果在氧化後的近地表覆蓋層沉積物和下層腐生物(包括返回的 RC343 孔)中返回了一些非常顯著的結果 27m @ 1.9 g/t 黃金 從水面上回來的 RC342 28m @ 1.8 g/t 金幣 從水面上回來的 RC375 20m @ 1.6 g/t 黃金 來自表面,包括 9m @ 1.7 g/t 黃金 還有返回的 RC376 15m @ 1.8 g/t 黃金 從 5 米深度開始(參見 2023 年 10 月 12 日和 2023 年 11 月 29 日的新聞稿)。
此處報告了九個螺旋孔,結果從 TR657 到 TR665(參見表 2 和圖 4 和 5)。
圖 4.地圖顯示了風化的基底腐殖巖中氧化物層和底層礦化帶限制的鎂金礦牀,以及從 TR658 到 TR665 的螺旋鑽孔的結果。條款;g/t = 克/噸,m = 米
第 553500 節
在 553500 段鑽了螺旋孔 TR665(圖 4 和 5,表 2)。先前對該部分的鑽石和反滲透鑽探已勾勒出一層層沉積物中持續礦化的區域,金含量約爲 0.5 g/t,例如,返回的 RC315 46m @ 0.5 g/t 黃金 還有返回的 RC134 26m @ 0.5 g/t 黃金)。
TR665 向東北鑽探得更遠,返回的黃金價值遠高於預期,包括 19 米 @ 1.3 克/噸黃金 來自表面,包括 2m @ 8.0 g/t 金幣 從 10 米深度開始。該洞以礦化而告終。這些結果表明,該部分的近地表層沉積物中存在比先前預期的更高品位的金礦化區域。
圖 5:穿過 MG 金礦牀的 553500 段顯示了近地表的氧化金腐石層和最近螺旋孔 TR665 的化驗結果,以及先前的 RC 和金剛石鑽孔的結果。術語;g/t = 克/噸,m = 米,ppm = 百萬分之一或克/噸
鑽孔 | 風化 | | | 來自 | 到 | 寬度 | 等級 |
# | | | | m | m | m | g/t 黃金 |
TR0657 | 毛毯/Saprolite | | | | | 0.0 | N.S.V。 |
| | 哎喲 | 20.0 | | | | |
TR0658 | 毛毯/Saprolite | | | 8.0 | 16.0 | 8.0 | 0.49 |
| | 哎喲 | 17.0 | | | | |
TR0659 | 毛毯/Saprolite | | | 2.0 | 18.0 | 16.0 | 0.37 |
| | 哎喲 | 18.0 | | | | |
TR0660 | 毛毯/Saprolite | | | 3.0 | 19.0 | 16.0 | 0.36 |
| | 哎喲 | 19.0 | | | | |
TR0661 | 毛毯/Saprolite | | | 8.0 | 16.0 | 8.0 | 0.32 |
| | 哎喲 | 20.0 | | | | |
TR0662 | 毛毯/Saprolite | | | 8.0 | 18.0 | 10.0 | 0.49 |
| | 哎喲 | 18.0 | | | | |
TR0663 | 毛毯/Saprolite | | | 0.0 | 20.0 | 20.0 | 0.34 |
| | 哎喲 | 20.0 | | | | |
TR0664 | 毛毯/Saprolite | | | 0.0 | 20.0 | 20.0 | 0.31 |
| | 哎喲 | 20.0 | | | | |
TR0665 | 毛毯/Saprolite | | | 0.0 | 19.0 | 19.0 | 1.26 |
| | | 包含 | 10.0 | 12.0 | 2.0 | 7.95 |
| | 哎喲 | 19.0 | | | | |
表 2:在 TR658 至 TR665 孔中,來自近地表的 MG 氧化金覆蓋層/腐蝕巖區域的螺旋鑽探結果。
條款;g/t = 克/噸,m = 米,N.S.V. = 無有效值
關於 Cabral Gold Inc.
該公司是一家初級資源公司,從事礦產的識別、勘探和開發,主要關注位於巴西的黃金地產。該公司持有位於巴西北部帕拉州塔帕霍斯地區的庫伊烏庫烏黃金區的100%權益。根據2022年10月12日的43-101號技術報告,Cuiué Cuiué項目迄今已確定了兩個主要的金礦牀,該項目包含符合國家儀器43-101標準的216萬噸 @ 0.87克/噸黃金(60.4萬盎司)的指示資源和1980萬噸 @ 0.84克/噸黃金(534,500盎司)的推斷資源。
塔帕霍斯黃金省是巴西曆史上規模最大的淘金熱的地點,根據ANM(Agencia Nacional de Mineracao 或巴西國家礦業局)的數據,該省在1978年至1995年間估計生產了3000萬至5000萬盎司的砂金。Cuiué Cuiuá是塔帕霍人最大的砂礦開採區,歷史上估計生產了2Moz的砂金。
欲了解更多信息,請聯繫:
“艾倫·卡特”
總裁兼首席執行官
Cabral Gold Inc.
電話:604.676.5660
Guillermo Hughes、MauSimm和FAIG. 是公司的顧問,也是國家儀器43-101所定義的合格人員,他們監督了本新聞稿中技術信息的準備工作。
多倫多證券交易所風險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。
前瞻性陳述
本新聞稿包含適用證券立法所指的某些前瞻性信息和前瞻性陳述(統稱 “前瞻性陳述”)。使用 “將”、“預期” 和類似表達方式旨在識別前瞻性陳述。這些陳述涉及已知和未知的風險、不確定性和其他因素,這些因素可能導致實際結果或事件與此類前瞻性陳述中的預期結果或事件存在重大差異。不應過度依賴此類前瞻性陳述。公司認爲,這些前瞻性陳述中反映的預期是合理的,但無法保證這些預期會被證明是正確的。
注意事項
金分析已通過 SGS 方法 FAA505(50 克電荷的火焰分析)進行,更高等級的樣本由 FAA525 檢查。分析質量由經過認證的參考文獻和空白進行監控。在發貨之前,樣品在公司勘探辦公室的監督下儲存。樣本由商業承包商運送到化驗實驗室。紙漿被歸還給公司並存檔。鑽孔結果以井下長度加權交叉點的形式引用。