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All Holes Drilled to Date Hit Broad Sulphide Mineralization Up to 135 Meters Wide* at Goliath’s Golddigger Property, Golden Triangle, B.C.
All Holes Drilled to Date Hit Broad Sulphide Mineralization Up to 135 Meters Wide* at Goliath’s Golddigger Property, Golden Triangle, B.C.
Infographic 1
Infographic 1Infographic 2
Infographic 2Infographic 3
Infographic 3New Extension Target drill highlights:
- 100% of all three drill holes completed to date on the New Extension Target at its Golddigger Property have intersected broad zones of significant sulphide mineralization up to 135 meters wide*. Assays are pending on all three holes and will be released once received, compiled, and interpreted.
- These significant intercepts confirm the presence of an extensive mineralizing system at depth and high potential for linear, widespread mineralized bodies that remain open in all directions.
- The type of mineralization (including semi-massive to massive pyrrhotite and pyrite), textures (including veining, stockwork and brecciation) and alteration (chloritization, silicification, epidotization) observed in the New Extension Target located in the underlying volcanics are similar to what has been observed in drill holes and at surface on the Surebet Zone located higher in the above sediments strongly suggesting the same extensive underlying feeder source for the mineralizing fluids.
- Drill hole GD-22-25 on Pad J in the New Extension Target intersected multiple broad intervals of disseminated and vein/breccia hosted sulphide mineralization of up to 95.5 meters wide* containing pyrrhotite, pyrite and chalcopyrite in Hazelton volcanics.
- Drill hole GD-22-26 on Pad J in the New Extension Target intersected a broad zone containing 135 meters wide* of vein/breccia-hosted and disseminated sulphide mineralization in Hazelton volcanic rocks from bedrock (30 m) to the end of the hole (165 m) consisting of pyrrhotite (up to 3%), chalcopyrite (up to 1%) and pyrite (up to 5%). The hole terminated in sulphide mineralization and remains open.
- A photo accompanying this announcement is available at
- Drill hole GD-22-27 on Pad J in the New Extension Target intersected a broad zone containing 108 meters wide* of sulphide veining and brecciation from bedrock (57 m) to 165 m consisting of pyrrhotite (5% overall, locally massive cm-wide sections), pyrite (1%, locally up to 3%) and chalcopyrite (trace, disseminated) and remains open.
- A photo accompanying this announcement is available at
- The extensive mineralizing system has been confirmed over 1 km North-South along the Surebet Zone and 2 km East-West from Real Deal to the newly drilled Pad J located in the New Extension Target that remains open in all directions; see map below.
- The drill rig from Pad J will be moved to Pad 15, 1.6 km to the West (820 m South of Real Deal) to target the Surebet system at depth while a second drill will start testing the extension of the system in the Hazelton volcanic rocks to the North at New Gold, 2.5 km to the North of Pad J (1 km north of North Rubble); see map below.
- This year's 24,000 meter planned drill program is designed to expand the extent of known mineralization from 2021 in all directions, including to the West (to Lake Pad, 940 m SW of Real Deal), test the known gold mineralization to the North (to New Gold, 1 km north of North Rubble), and to the East (to Pad J within the New Extension Target, 1.5 Km South-East of the Surebet encompassing an area of 5.25 square km. Outcrop where initial drilling have confirmed multiple broad zones of mineralization); see map below.
- The 2022 drill program will focus on expanding the known parameters of the Surebet high-grade gold-silver discovery with 24,000 m of drilling planned in 84 holes from 24 pad locations using 4 drill rigs. It's designed for resource level infill drilling and outline the large mineralized system over an area of 2.1 km East-West by 2.5 km North-South (5.25 square kilometers).
- A photo accompanying this announcement is available at
TORONTO, June 28, 2022 (GLOBE NEWSWIRE) -- Goliath Resources Limited (TSX-V: GOT) (OTCQB: GOTRF) (FSE: B4IF) (the "Company" or "Goliath") is pleased to report observations from the drilling completed from its J Pad location on the Extension Target on the Surebet discovery at its 100% controlled Golddigger Property (the "Property"), Golden Triangle, B.C. All three drill holes completed to date on the New Extension Target have returned significant intervals of sulphide mineralization up to 135 meters*. They consist of stringers and aggregations of semi-massive to massive pyrrhotite, chalcopyrite and pyrite within veins, stockwork and breccia. Sulphide mineralization has been observed throughout the drill holes and remains open.
The type of mineralization (including semi-massive to massive pyrrhotite and pyrite), textures (including veining, stockwork and brecciation) and alteration (chloritization, silicification, epidotization) observed in the New Extension Target located in the underlying volcanics are similar to what has been observed in drill holes and at surface on the Surebet Zone located higher in the above sediments strongly suggesting the same extensive underlying feeder source for the mineralizing fluids. Mineralization in the New Extension Target is hosted in Hazelton volcanic rocks (strongly altered plagioclase-phyric andesite) and in veins/breccia within the andesite. In comparison, mineralization in the Surebet Zone is mainly hosted in a shear zone cutting Hazelton sediments. Due to the difference in host rock composition (particularly the lower amount of Ca and Mg in the sediments compared to the andesite) and rock competence, the type of alteration and structures developed differ between the different host rocks even though they are probably part of the same system.
GD-22-26 (azimuth 040°; dip -55°) and GD-22-27 (azimuth 150°; dip -55°) were collared from Pad J, the most easterly pad planned for 2022 in the Extension Target, located 1.5 km Southeast of the outcropping Surebet and 2 km East from Real Deal; see map above.
Drill hole GD-22-26
Drill hole GD-22-26 (E 458908.947, N 6161976.043, azimuth 040°; dip -55°) intercepted 135 m* of sulphide mineralized andesite from bedrock (30 m) to the bottom of the hole (165 m). Mineralization primarily occurs as millimeter- to centimeter-size stringers and aggregations of sulphides within quartz and quartz-chlorite-epidote veins and breccia throughout a strongly epidotized andesitic volcanic host rock and as disseminated grains throughout the andesite. The majority of the mineralization consists of pyrrhotite (3% overall, locally massive cm-wide sections), pyrite (3%, locally up to 5%) and chalcopyrite (in aggregations). Pyrrhotite is common in the entire hole where it occurs as stringers and aggregations within strongly silicified domains that also contain chlorite and epidote and disseminated within the host rock. At 84.79 meters and 134.78 meters brecciated sections with semi-massive to massive pyrrhotite up to 2 cm wide have been observed. Chalcopyrite aggregations are more common in quartz vein/breccia domains that usually extend for <0.3 m and rarely occur as fine-grained aggregations and disseminated in the silicified domain surrounding quartz vein/breccia. Pyrite occurs throughout the andesitic volcanic rocks as disseminated crystal up to 5 mm in size. The host rock observed in the core of drill hole GD-22-26 consists of a plagioclase-phyric andesite with strong epidote, chlorite and silica alteration intervals surrounding veins, vein stockwork and breccia that generally extend for several meters. The epidote alteration and textures in combination with the chloritization, silica alteration, quartz veining and sulphide precipitation all point at fluid movement through the rock; see photos above.
The last 10 m of the hole contain less than 2% sulphides overall. However, abundant quartz-chlorite veining and epidote alteration persists to end of hole suggesting that the mineralization remains open to depth.
The hole targeted surface mineralization including a channel cut that assayed 6.7 gpt Au over 0.33 m and grab samples that returned up to 4.78 gpt Au. These surface samples consist of quartz-breccia containing semi-massive to massive galena, chalcopyrite, pyrrhotite and pyrite.
Drill hole GD-22-27
Drill hole GD-22-27 (E 458908.947, N 6161976.043, azimuth 150°; dip -55°) intercepted 108 m* of sulphide mineralization hosted in a strongly altered andesite from bedrock (57 m) to 165 m. Mineralization occurs as stringers, veins and disseminated and mainly consists of pyrrhotite and pyrite, with minor chalcopyrite. Similarly to drill hole GD-22-26, mineralization primarily occurs as millimeter- to centimeter-stringers and aggregations of sulphides within quartz and quartz-chlorite-epidote veins and breccia throughout a strongly epidotized andesitic volcanic host rock and as disseminated grains throughout the andesite. Most of the mineralization consists of pyrrhotite (5% overall, locally massive cm-wide sections), pyrite (1 %, locally up to 3 %) and chalcopyrite (trace, disseminated). Pyrrhotite is common in the entire hole where it occurs as stringers and aggregations within strongly silicified domains that also contain chlorite and disseminated within the host rock. GD-22-27 contains a higher percentage of disseminated pyrrhotite and pyrrhotite-chlorite veining within the epidote altered andesite host rock compared to holes GD-22-25 and GD-22-26. Throughout the core, the mineralized andesitic rocks show patchy epidote alteration generally associated with micro veining and fractures containing sulphide mineralization and quartz-chlorite. In drill hole GD-22-27 sulphide mineralization intensity is higher near the top and down to 150 m depth. These intercepts correlate with similar intercepts on all holes drilled from Pad J to date, presenting the high potential for linear, widespread mineralized bodies at depth; see photos above.
Drill Hole GD-22-27 targeted surface mineralization including a channel cut that run 13.5 gpt Au over 0.58 m and grab samples up to 44.4 gpt Au. These surface samples consist of quartz breccia containing semi-massive to massive galena, chalcopyrite, pyrrhotite and pyrite.
2022 drill campaign
The drill rig from Pad J will be moved to Pad 15, 1.6 km to the West (820 m South of Real Deal) to target the Surebet system at depth while a second drill will start testing the extension of the system in the Hazelton volcanic rocks to the North at New Gold, 2.5 km to the North of Pad J (1 km north of North Rubble); see map above.
During the 2022 drill campaign, Goliath plans to test the Surebet mineralized system at depth over an extensive area reaching as far as Lake Pad to the West (940 m SW of Real Deal) and New Gold to the North (1 km north of North Rubble) focused on delineating a mineralized area of 2.1 km East-West by 2.5 km North-South; see map above. Several drill locations are planned up to 600 meters West of Real Deal to target the Surebet mineralized system at depth based on the projected model generated from the 2021 drill results and 2020 channel sample results. Multiple surface channel, chip and grab samples collected from Real Deal and Cloud 9 secondary structures believed to be associated with the Surebet Zone returned significant gold and silver values, further confirming the presence of a large gold-silver rich mineralizing system at depth. These secondary structures are interpreted to be acting as conduits for fluids to the surface. A series of drill holes are planned for the New Gold zone located 1 km North of Surebet. Similarly to the New Extension Target, this zone contains surface gold mineralization over 400 meters that remains open with ~ 30 m of gold bearing breccia observed in outcrop. The New Gold Zone is hosted in Hazelton volcanics in close proximity to the 'Red Line'. The majority of the world class mineral deposits discovered within the Golden Triangle are hosted in the Hazelton volcanics and occur within a few kilometers of the unconformity between Lower Hazelton and Stuhini rocks (also known as the 'Red Line').
Roger Rosmus, Founder and CEO of Goliath Resources, states: "Drilling on the Extension Target keeps delivering exciting results with 100% of holes intersecting significant intervals of sulphide mineralization reiterating the presence of a large mineralizing system at play on the Golddigger property. Goliath is looking forward to the weeks to come as the 24,000 m drill program moves forward and new information and data becomes available to better define the extent of this extensive mineralizing system at Surebet."
Golddigger Property
The Golddigger Property is 100 % controlled covering an area of 23,859 hectares (59,646 acres or 239 square-kilometers) and is in the world class geological setting of the Eskay Rift within the Golden Triangle of British Columbia and within 2 km of the 'Red Line' that is host to multiple world class deposits. The property is on tide water 30 kilometers southeast of Stewart, British Columbia.
Surebet is characterized by a series of NW-SE trending structures that occur within a package of Hazelton Group sediments underlain by Hazelton volcanics and are within a few kilometers of the Red Line. All 24 diamond drill holes completed in 2021 intersected significant intervals of Au-Ag polymetallic mineralization over 1 km of strike, 1.1 km down-dip and 600 meters of vertical relief. Drill hole GD-21-03* intersected 6.37 gpt AuEq (4.46 gpt Au and 122.13 gpt Ag) over 35.72 meters and drill hole GD-21-05* intersected 12.6 gpt AuEq (8.06 gpt Au and 313.66 gpt Ag) over 6.38 meters. The average grade and width from all 24 holes* assayed 6.29 gpt AuEq (4.35 gpt Au and 104.94 gpt Ag) over 5.87 meters, respectively.
LiDAR imagery, drone imagery, and field observations have identified several additional paralleling structures within a 4 square-kilometers area. Geochemical analyses have confirmed high-grade gold-silver polymetallic mineralization within these structures. The steeply dipping Real Deal and Cloud 9 structures, as well as the off-shoot structures from the Extension Zone, display similar mineralization, geochemistry and textures to the Surebet Zone. Geologic observations at surface and within drill core show structural strain concentrating in the Surebet Zone along its shallower-dipping geometry. Real Deal and Cloud 9 are believed to be en-echelon structures that connect with Surebet at depth. The mineralized Surebet Zone remains open in all directions.
Qualified Person
Rein Turna P. Geo is the qualified person as defined by National Instrument 43-101, for Goliath Resource Limited projects, and supervised the preparation of, and has reviewed and approved, the technical information in this release.
Other
All rock, channel and talus fine samples were crushed and pulverized at MSALABS's laboratory in Terrace, BC. MSALABS is either Certified to ISO 9001:2008 or Accredited to ISO 17025:2005 in all of its locations. The resulting sample pulps were analyzed for gold by fire assay and metallic screen fire assay in Langley, BC. The pulps were also assayed using multi-element aqua regia digestion at MSALABS's laboratory in Langley, BC. The coarse reject portions of the rock samples, as well as the pulps, were shipped to Goliath Resources Ltd.'s storage facility in Terrace, BC. All samples were analyzed using MSALABS's assay procedure ICP-130, a 1:1:1 aqua regia digestion with inductively-coupled plasma atomic emission spectrometry (ICP-AES) or inductively-coupled plasma mass spectrometry (ICP-MS) finish for 35 elements as well as the FAS-121 lead collection fire assay fusion procedure with atomic absorption spectroscopy (AAS) finish. Any results greater than 100 ppm for silver or 10,000 ppm copper, lead and zinc were additionally assayed using MSALABS's ICA-6xx method particular to each element. This method used an HNO3-HCl digestion followed by ICP-AES (or titrimetric and gravimetric analysis). Gold values of greater than 10 ppm Au were assayed by the FAS-425 method which includes a fire-assay fusion procedure with a gravimetric finish. Samples with Au greater than 5 ppm were additionally analyzed using metallic screen fire assay with MSALABS's MSC-150 or MSC-350 method. QA/QC samples including blanks, standards, and duplicate samples were inserted regularly into the sample sequence.
The reader is cautioned that grab samples are spot samples which are typically, but not exclusively, constrained to mineralization. Grab samples are selective in nature and collected to determine the presence or absence of mineralization and are not intended to be representative of the material sampled.
About Goliath Resources Limited
Goliath Resources Limited is an explorer of precious metals projects in the prolific Golden Triangle of northwestern British Columbia and Abitibi Greenstone Belt of Quebec. All of its projects are in world class geological settings and geopolitical safe jurisdictions amenable to mining in Canada.
For more information please contact:
Goliath Resources Limited
Mr. Roger Rosmus
Founder and CEO
Tel: +1-416-488-2887 x222
roger@goliathresources.com
* Widths are reported in drill core lengths and the true widths are not known and AuEq metal values are calculated using: Au 1792.60 USD/oz, Ag 23.13 USD/oz, Cu 4.37 USD/lbs, Pb 1.05 USD/lbs and Zn 1.52 USD/lbs on November 28, 2021. There is potential for economic recovery of gold, silver, copper, lead, and zinc from these occurrences based on other mining and exploration projects in the same Golden Triangle Mining Camp where Goliath's project is located such as the Homestake Ridge Gold Project (Auryn Resources Technical Report, Updated Mineral Resource Estimate and Preliminary Economic Assessment on the Homestake Ridge Gold Project, prepared by Minefill Services Inc. (Bothell, Washington), dated May 29, 2020. Here, AuEq values were calculated using 3-year running averages for metal price, and included provisions for metallurgical recoveries, treatment charges, refining costs, and transportation. Recoveries for Gold were 85.5%, Silver at 74.6%, Copper at 74.6% and Lead at 45.3%. It will be assumed that Zinc can be recovered with the Copper at the same recovery rate of 74.6%. The quoted reference of metallurgical recoveries is not from Goliath's Golddigger Project, Surebet Zone mineralization, and there is no guarantee that such recoveries will ever be achieved, unless detailed metallurgical work such as in a Feasibility Study can be eventually completed on the Golddigger Project.
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange), nor the OTCQB Venture Market accepts responsibility for the adequacy or accuracy of this release.
Certain statements contained in this press release constitute forward-looking information. These statements relate to future events or future performance. The use of any of the words "could", "intend", "expect", "believe", "will", "projected", "estimated" and similar expressions and statements relating to matters that are not historical facts are intended to identify forward-looking information and are based on Goliath's current belief or assumptions as to the outcome and timing of such future events. Actual future results may differ materially. In particular, this release contains forward-looking information relating to, among other things, the ability of Company to complete the financings and its ability to build value for its shareholders as it develops its mining properties. Various assumptions or factors are typically applied in drawing conclusions or making the forecasts or projections set out in forward-looking information. Those assumptions and factors are based on information currently available to Goliath. Although such statements are based on management's reasonable assumptions, there can be no assurance that the proposed transactions will occur, or that if the proposed transactions do occur, will be completed on the terms described above.
The forward-looking information contained in this release is made as of the date hereof and Goliath is not obligated to update or revise any forward-looking information, whether as a result of new information, future events or otherwise, except as required by applicable securities laws. Because of the risks, uncertainties and assumptions contained herein, investors should not place undue reliance on forward-looking information. The foregoing statements expressly qualify any forward-looking information contained herein.
This announcement does not constitute an offer, invitation, or recommendation to subscribe for or purchase any securities and neither this announcement nor anything contained in it shall form the basis of any contract or commitment. In particular, this announcement does not constitute an offer to sell, or a solicitation of an offer to buy, securities in the United States, or in any other jurisdiction in which such an offer would be illegal.
The securities referred to herein have not been and will not be will not be registered under the United States Securities Act of 1933, as amended (the "U.S. Securities Act"), or any state securities laws and may not be offered or sold within the United States or to or for the account or benefit of a U.S. person (as defined in Regulation S under the U.S. Securities Act) unless registered under the U.S. Securities Act and applicable state securities laws or an exemption from such registration is available.
NOT FOR DISSEMINATION IN THE UNITED STATES OR FOR DISTRIBUTION TO U.S. NEWSWIRE SERVICES AND DOES NOT CONSTITUTE AN OFFER OF THE SECURITIES DESCRIBED HEREIN.
信息圖1
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信息圖2信息圖3
信息圖3新的擴展目標演練重點:
- 截至目前,在其Golddigger物業的新擴展目標上完成的所有三個鑽孔100%都與寬達135米的廣泛硫化物礦化帶相交*。所有三個洞的化驗都在等待進行,一旦收到、編譯和解釋,就會公佈。
- 這些重要的截獲證實了在深部存在廣泛的礦化系統,以及在各個方向保持開放的線性、廣泛的礦化體的高潛力。
- 在位於下伏火山巖中的新延伸靶區觀察到的礦化類型(包括半塊狀至塊狀磁黃鐵礦和黃鐵礦)、結構(包括脈狀、網狀和角礫化)和蝕變(綠泥化、硅化、綠簾化)與在上述沉積物中較高的Surebet帶的鑽孔和地表觀察到的相似,強烈表明成礦流體的廣泛下伏來源相同。
- 在新延伸目標的J墊上的GD-22-25鑽孔與多個廣泛的浸染性和脈狀/角礫巖賦存的硫化物礦化相交,該礦化寬達95.5米*,在黑茲爾頓火山巖中含有磁黃鐵礦、黃鐵礦和黃銅礦。
- 位於新延伸目標的鑽頭J上的鑽孔GD-22-26穿過一個寬闊的區域*,其中包含135米寬*的脈狀/角礫巖容礦和浸染硫化物礦化,從基巖(30米)到孔底(165米),由磁黃鐵礦(高達3%)、黃銅礦(高達1%)和黃鐵礦(高達5%)組成。這個洞終止於硫化物礦化,並保持敞開。
- 這一公告附帶的照片可在以下網址查閲
- 在新延伸目標的J墊上的GD-22-27鑽孔穿過一個寬闊的區域,從基巖(57米)到165米,包含108米寬*的硫化物脈狀和角礫巖,由磁黃鐵礦(總體5%,局部塊狀釐米寬的切片),黃鐵礦(1%,局部高達3%)和黃銅礦(微量,浸染)組成,並保持開放狀態。
- 這一公告附帶的照片可在以下網址查閲
- 廣泛的成礦系統已被證實,沿Surebet區南北方向超過1公里,從Real Deal到位於新延伸目標的新鑽探的Pad J東西方向2公里,該延伸目標仍然四通八達;見下圖。
- Pad J的鑽機將被移到Pad 15,向西1.6公里(Real Deal以南820米),以確定Surebet系統的深度,而第二次鑽探將開始測試該系統在Hazelton火山巖中向北延伸到New Gold,Pad J以北2.5公里(北瓦礫以北1公里);見下圖。
- 今年24,000米的計劃鑽探計劃旨在從2021年起全方位擴大已知礦化範圍,包括向西(至萊德湖,Real Deal西南940米),向北(至New Gold,北碎石以北1公里)和向東(至新延伸目標內的Pad J,Surebet東南1.5公里,面積5.25平方公里)。初步鑽探已確認多個廣泛礦化帶的露頭);見下圖。
- 2022年的鑽探計劃將重點擴大Surebet高品位金銀髮現的已知參數,計劃使用4個鑽機在24個墊地位置的84個孔中鑽探24,000米。它是為資源級加密鑽探而設計的,並勾勒出東西長2.1公里,南北長2.5公里(5.25平方公里)的大型礦化系統。
- 這一公告附帶的照片可在以下網址查閲
多倫多,2022年6月28日(環球通訊社)--Goliath Resources Limited(多倫多證券交易所股票代碼:GOT)(OTCQB:GOTRF)(FSE:B4IF)(“公司”或《歌利亞》)很高興地報告從其在Surebet發現的Surebet發現的延伸目標上的J Pad位置完成的鑽探觀察到其100%控制的Golddigger物業(The“財產”),不列顛哥倫比亞省金三角。到目前為止,在新延伸目標上完成的所有三個鑽孔都返回了長達135米*的大量硫化物礦化區間。它們由脈狀、網狀和角礫巖中的半塊狀至塊狀磁黃鐵礦、黃銅礦和黃鐵礦組成的串狀和集合體組成。在整個鑽孔中觀察到硫化物礦化作用,並保持開放狀態。
在位於下伏火山巖中的新延伸靶區觀察到的礦化類型(包括半塊狀至塊狀磁黃鐵礦和黃鐵礦)、結構(包括脈狀、網狀和角礫化)和蝕變(綠泥化、硅化、綠簾化)與在上述沉積物中較高的Surebet帶的鑽孔和地表觀察到的相似,強烈表明成礦流體的廣泛下伏來源相同。新延伸靶區的礦化賦存於黑茲爾頓火山巖(強烈蝕變的斜長-千粒狀安山巖)和安山巖內的脈狀/角礫巖中。相比之下,Surebet帶的礦化主要賦存於切割黑茲爾頓沉積物的剪切帶中。由於寄主巖石組成(特別是沉積物中的鈣、鎂含量低於安山巖)和巖石能力的不同,不同的寄主巖石之間的蝕變類型和發育的構造也不同,儘管它們可能是同一系統的一部分。
GD-22-26(方位角040°;傾角-55°)和GD-22-27(方位角150°;傾角-55°)是從2022年計劃在延伸目標中最東側的墊層Pad J上翻領的,位於露頭Surebet東南1.5公里,Real Deal以東2公里處;見上圖。
GD-22-26鑽孔
GD-22-26鑽孔(E 458908.947,N 6161976.043,方位角0 40°;傾角-55°)從基巖(30m)到井底(165m)截留硫化物礦化安山巖135m*。礦化主要以毫米至釐米大小的硫化物串狀和集合體的形式出現在石英和石英-綠泥石-綠簾石脈體和角礫巖中,貫穿於強烈的綠簾化安山巖主巖中,並以瀰漫在安山巖中的顆粒形式出現。大多數礦化由磁黃鐵礦(總體3%,局部塊狀釐米寬的切片)、黃鐵礦(3%,局部高達5%)和黃銅礦(集合體)組成。磁黃鐵礦在整個孔洞中很常見,它以串狀和集合體的形式出現在高度硅化的區域中,這些區域也含有綠泥石和綠簾石,並散佈在主巖中。在84.79m和134.78米處,觀察到了寬達2釐米的半塊狀到塊狀磁黃鐵礦的角礫狀剖面。黃銅礦聚集體在石英脈/角礫巖域中更為常見,通常延伸到
這個洞的最後10米含有不到2%的硫化物。然而,豐富的石英-綠泥石脈狀和綠簾石蝕變一直持續到孔底,表明礦化仍向深部開放。
該洞以地表礦化為目標,包括一個渠道切割,在0.33米範圍內分析6.7gpt Au,並抓取高達4.78gpt Au的樣品。地表樣品由含半塊至塊狀方鉛礦、黃銅礦、磁黃鐵礦和黃鐵礦的石英角礫巖組成。
GD-22-27鑽孔
鑽孔GD-22-27(E 458908.947,N 6161976.043,方位150°;傾角-55°)截留了108m*的硫化物礦化,賦存於基巖(57m)至165m的強烈蝕變安山巖中。礦化呈串狀、脈狀,呈浸染狀分佈,主要由磁黃鐵礦和黃鐵礦組成,並有少量黃銅礦。與GD-22-26鑽孔相似,礦化主要以毫米至釐米級的串狀硫化物和硫化物聚集體的形式出現在石英和石英-綠泥石-綠簾石脈體和角礫巖中,遍及強烈綠簾化的安山質火山主巖,並以瀰漫在安山巖中的顆粒形式出現。大多數礦化由磁黃鐵礦(總體5%,局部塊狀釐米寬的切片)、黃鐵礦(1%,局部高達3%)和黃銅礦(微量,浸染)組成。磁黃鐵礦在整個孔洞中很常見,它以串狀和集合體的形式出現在高度硅化的區域中,這些區域也含有綠泥石,並分散在主巖中。與GD-22-25和GD-22-26孔相比,GD-22-27孔中綠簾石蝕變安山巖中含有較高比例的浸染型磁黃鐵礦和磁黃鐵礦-綠泥石脈。在整個巖芯,礦化安山巖表現為斑片狀綠簾石蝕變,通常與含有硫化物礦化和石英綠泥石的微脈和裂縫有關。在GD-22-27鑽孔中,硫化物礦化強度在頂部附近較高,向下達150m。這些截距與迄今為止從Pad J鑽出的所有孔上的類似截距相關聯,表明在深處存在廣泛的線狀礦化體的高潛力;見上圖。
鑽孔GD-22-27以地表礦化為目標,包括一個超過0.58米、長13.5gpt Au的渠道切割,並抓取高達44.4gpt Au的樣品。地表樣品由含半塊至塊狀方鉛礦、黃銅礦、磁黃鐵礦和黃鐵礦的石英角礫巖組成。
2022年演練活動
Pad J的鑽機將被移到Pad 15,向西1.6公里(Real Deal以南820米),以確定Surebet系統的深度,而第二次鑽探將開始測試該系統在Hazelton火山巖中向北延伸到New Gold,Pad J以北2.5公里(北瓦礫以北1公里);見上圖。
在2022年的鑽探活動中,Goliath計劃對Surebet礦化系統進行深度測試,覆蓋範圍廣泛,西至萊德湖(Real Deal西南940米),北至New Gold(北瓦礫以北1公里),重點是劃定東西2.1公里、南北2.5公里的礦化區;見上圖。根據2021年鑽探結果和2020年渠道樣本結果生成的預測模型,計劃在Real Deal以西600米處規劃幾個鑽探地點,以瞄準Surebet礦化系統的深度。從被認為與Surebet帶有關的Real Deal和Cloud 9次級構造中採集的多個地表通道、芯片和Grab樣品返回了顯著的金銀價值,進一步證實了深部存在一個大型的富含金銀的礦化系統。這些二級結構被解釋為充當流體進入地表的管道。位於Surebet以北1公里處的新金礦區計劃進行一系列鑽探。與新延伸目標相似,該帶包含400米以上的地表金礦化,保持開放狀態,露頭觀察到約30米的含金角礫巖。新黃金區位於黑茲爾頓火山巖中,非常接近紅線。在金三角內發現的大多數世界級礦藏賦存於黑茲爾頓火山巖中,位於下黑茲爾頓巖石和斯圖希尼巖石之間不整合(也稱為紅線)幾公里範圍內。
Goliath Resources創始人兼首席執行官羅傑·羅斯穆斯表示:對擴展目標的鑽探不斷帶來令人興奮的結果有100%的孔相交明顯的硫化物礦化間隔,重申了在Golddigger礦藏上存在一個大型礦化系統。Goliath期待着未來幾周,因為24,000米的鑽探計劃取得進展,新的信息和數據可以更好地確定Surebet這一廣泛礦化系統的範圍。“
Golddigger屬性
Golddigger地產100%控制,佔地23,859公頃(59,646英畝或239平方公里),位於不列顛哥倫比亞省金三角內世界級地質環境的Eskay裂谷,距離擁有多個世界級礦藏的紅線不到2公里。該房產位於不列顛哥倫比亞省斯圖爾特東南30公里處的潮水上。
Surebet以一系列NW-SE向構造為特徵,這些構造賦存於黑茲爾頓火山之下的哈澤爾頓羣沉積物中,距離紅線不到幾公里。2021年完成的所有24個鑽石鑽孔都與Au-Ag多金屬礦化的重要區間相交,走向超過1公里,向下傾斜1.1公里,垂直起伏600米。鑽孔GD-21-03*與6.37gpt AuEq(4.46gpt Au和122.13 gpt Ag)相交超過35.72米,而GD-21-05*鑽孔與12.6gpt AuEq(8.06gpt Au和313.66 gpt Ag)相交超過6.38米。所有24個孔的平均品位和寬度分別為6.29gpt AuEq(4.35gpt Au和104.94 gpt Ag)。
激光雷達圖像、無人機圖像和現場觀察已經在4平方公里的區域內發現了幾個額外的平行結構。地球化學分析證實,這些構造中存在高品位的金銀多金屬礦化。陡峭傾斜的Real Deal和Cloud 9構造,以及來自延伸帶的副射構造,顯示出與Surebet帶相似的礦化、地球化學和結構。地表和鑽芯內的地質觀察表明,Surebet帶沿其較淺的傾斜幾何結構,構造應變集中。Real Deal和Cloud 9被認為是與Surebet深度相連的梯隊結構。礦化的Surebet帶仍向四面八方開放。
有資格的人
Rein Turna P.Geo是國家儀器43-101定義的Goliath資源有限項目的合格人員,並監督本新聞稿中技術信息的準備,並已進行審查和批准。
其他
在不列顛哥倫比亞省泰瑞斯的MSALABS實驗室,所有的巖石、水道和距骨細小樣品都被粉碎和粉碎。MSALABS在其所有地點都通過了ISO9001:2008認證或ISO 17025:2005認證。在不列顛哥倫比亞省蘭利市,用火試紙法和金屬屏火法對所得樣品紙漿中的金進行了分析。這些牙髓也在不列顛哥倫比亞省蘭利的MSALABS實驗室用多元素王水消化法進行了檢測。粗略的巖石樣本和紙漿一起被運往哥利亞資源有限公司位於不列顛哥倫比亞省泰瑞斯的儲存設施。所有樣品均採用MSALABS的分析程序ICP-130、1:1:1王水消解-電感耦合等離子體原子發射光譜分析(ICP-AES)或電感耦合等離子體質譜(ICP-MS)分析,以及Fas-121鉛收集火焰分析結合原子吸收光譜分析(AAS)分析程序。任何超過100ppm的銀或10000ppm的銅、鉛和鋅的結果都使用MSALABS針對每種元素的ICA-6xx方法進行額外檢測。該方法採用硝酸-鹽酸消解,然後進行電感耦合等離子體發射光譜分析(或滴定和重量分析)。金值大於10ppm的金是用Fas-425方法測定的,該方法包括重量分析熔融程序。另外,用MSALABS的MSC-150或MSC-350方法對Au大於5ppm的樣品進行金屬屏蔽火分析。將包括空白、標準和重複樣品的QA/QC樣品定期插入到樣品序列中。
讀者需要注意的是,抓取樣本是典型的、但不完全限於礦化的斑點樣本。GRAB樣品是選擇性的,收集的目的是確定礦化的存在或不存在,並不是為了代表所採樣的材料。
關於歌利亞資源有限公司
Goliath Resources Limited是一家貴金屬項目勘探商,位於不列顛哥倫比亞省西北部多產的金三角和魁北克省Abitibi Greenstone帶。它的所有項目都位於世界級的地質環境和地緣政治安全管轄區,適合在加拿大進行採礦。
如需更多信息,請聯繫:
歌利亞資源有限公司
羅傑·羅斯穆斯先生
創始人兼首席執行官
電話:+1-416-488-2887 x222
郵箱:roger@goliathresource ces.com
* 寬度是以鑽芯長度報告的,真實寬度是未知的,AUEQ金屬價值的計算方法為:2021年11月28日的Au 1792.60美元/盎司,Ag23.13美元/盎司,Cu4.37美元/磅,Pb1.05美元/磅和Zn1.52美元/磅。基於Goliath項目所在同一金三角礦營的其他採礦和勘探項目,如Homestake Ridge金礦項目(Auryn Resources技術報告、最新礦產資源估計和Homestake Ridge金礦項目的初步經濟評估),從這些礦石中經濟回收金、銀、銅、鉛和鋅的潛力很大。在這裏,AuEq值是使用金屬價格的三年運行平均值計算的,其中包括冶金回收、處理費用、精煉成本和運輸撥備。金、銀、銅、鉛的回收率分別為85.5%、74.6%、74.6%、45.3%。假設鋅與銅的回收率相同,為74.6%。所引用的冶金回收不是來自Goliath的Golddigger項目,Surebet帶礦化,也不能保證永遠會實現這樣的回收,除非最終能夠完成Golddigger項目的詳細冶金工作,如可行性研究中的工作。
多倫多證券交易所及其監管服務提供商(該術語在多倫多證券交易所的政策中定義)和OTCQB風險市場均不對本新聞稿的充分性或準確性承擔責任。
本新聞稿中包含的某些陳述屬於前瞻性信息。這些陳述與未來的事件或未來的表現有關。使用“可能”、“打算”、“預期”、“相信”、“將會”、“預計”、“估計”以及與非歷史事實有關的類似表述和陳述,意在識別前瞻性信息,並基於歌利亞目前對此類未來事件的結果和時機的信念或假設。未來的實際結果可能會有很大不同。特別是,本新聞稿包含與公司完成融資的能力以及在開發其採礦資產時為股東創造價值的能力等相關的前瞻性信息。在得出結論或作出前瞻性信息中列出的預測或預測時,通常會應用各種假設或因素。這些假設和因素是基於歌利亞目前掌握的信息。雖然該等陳述是基於管理層的合理假設,但不能保證建議的交易將會發生,或如果建議的交易確實發生,將按上述條款完成。
本新聞稿中包含的前瞻性信息是截至本文發佈之日的,除非適用的證券法要求,否則歌利亞沒有義務因新信息、未來事件或其他原因而更新或修改任何前瞻性信息。由於本文包含的風險、不確定性和假設,投資者不應過度依賴前瞻性信息。上述陳述明確表示,本文中包含的任何前瞻性信息都是合格的。
本公告不構成認購或購買任何證券的要約、邀請或推薦,本公告或其中包含的任何內容均不構成任何合同或承諾的基礎。特別是,本公告不構成在美國或任何其他司法管轄區出售或邀請購買證券的要約,在這些司法管轄區,此類要約是非法的。
本文提及的證券尚未、也不會根據修訂後的1933年美國證券法(“美國證券法”)或任何州證券法進行註冊,且不得在美國境內或為美國個人的賬户或利益(如美國證券法下的S規則所定義)提供或出售,除非根據美國證券法和適用的州證券法註冊,或獲得此類註冊豁免。
不得在美國傳播或分發給美國新聞通訊社服務,也不構成本文所述證券的要約。
moomoo是Moomoo Technologies Inc.公司提供的金融資訊和交易應用程式。
在美國,moomoo上的投資產品和服務由Moomoo Financial Inc.提供,一家受美國證券交易委員會(SEC)監管的持牌主體。 Moomoo Financial Inc.是金融業監管局(FINRA)和證券投資者保護公司(SIPC)的成員。
在新加坡,moomoo上的投資產品和服務是通過Moomoo Financial Singapore Pte. Ltd.提供,該公司受新加坡金融管理局(MAS)監管(牌照號碼︰CMS101000) ,持有資本市場服務牌照 (CMS) ,持有財務顧問豁免(Exempt Financial Adviser)資質。本內容未經新加坡金融管理局的審查。
在澳大利亞,moomoo上的金融產品和服務是通過Futu Securities (Australia) Ltd提供,該公司是受澳大利亞證券和投資委員會(ASIC)監管的澳大利亞金融服務許可機構(AFSL No. 224663)。請閱讀並理解我們的《金融服務指南》、《條款與條件》、《隱私政策》和其他披露文件,這些文件可在我們的網站 https://www.moomoo.com/au中獲取。
在加拿大,透過moomoo應用程式提供的僅限訂單執行的券商服務由Moomoo Financial Canada Inc.提供,並受加拿大投資監管機構(CIRO)監管。
在馬來西亞,moomoo上的投資產品和服務是透過Moomoo Securities Malaysia Sdn. Bhd. 提供,該公司受馬來西亞證券監督委員會(SC)監管(牌照號碼︰eCMSL/A0397/2024) ,持有資本市場服務牌照 (CMSL) 。本內容未經馬來西亞證券監督委員會的審查。
Moomoo Technologies Inc., Moomoo Financial Inc., Moomoo Financial Singapore Pte. Ltd.,Futu Securities (Australia) Ltd, Moomoo Financial Canada Inc和Moomoo Securities Malaysia Sdn. Bhd., 是關聯公司。
風險及免責聲明
moomoo是Moomoo Technologies Inc.公司提供的金融資訊和交易應用程式。
在美國,moomoo上的投資產品和服務由Moomoo Financial Inc.提供,一家受美國證券交易委員會(SEC)監管的持牌主體。 Moomoo Financial Inc.是金融業監管局(FINRA)和證券投資者保護公司(SIPC)的成員。
在新加坡,moomoo上的投資產品和服務是通過Moomoo Financial Singapore Pte. Ltd.提供,該公司受新加坡金融管理局(MAS)監管(牌照號碼︰CMS101000) ,持有資本市場服務牌照 (CMS) ,持有財務顧問豁免(Exempt Financial Adviser)資質。本內容未經新加坡金融管理局的審查。
在澳大利亞,moomoo上的金融產品和服務是通過Futu Securities (Australia) Ltd提供,該公司是受澳大利亞證券和投資委員會(ASIC)監管的澳大利亞金融服務許可機構(AFSL No. 224663)。請閱讀並理解我們的《金融服務指南》、《條款與條件》、《隱私政策》和其他披露文件,這些文件可在我們的網站 https://www.moomoo.com/au中獲取。
在加拿大,透過moomoo應用程式提供的僅限訂單執行的券商服務由Moomoo Financial Canada Inc.提供,並受加拿大投資監管機構(CIRO)監管。
在馬來西亞,moomoo上的投資產品和服務是透過Moomoo Securities Malaysia Sdn. Bhd. 提供,該公司受馬來西亞證券監督委員會(SC)監管(牌照號碼︰eCMSL/A0397/2024) ,持有資本市場服務牌照 (CMSL) 。本內容未經馬來西亞證券監督委員會的審查。
Moomoo Technologies Inc., Moomoo Financial Inc., Moomoo Financial Singapore Pte. Ltd.,Futu Securities (Australia) Ltd, Moomoo Financial Canada Inc和Moomoo Securities Malaysia Sdn. Bhd., 是關聯公司。
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