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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.
信息图1
信息图1信息图2
信息图2信息图3
信息图3新的扩展目标演练重点:
- 截至目前,在其Golddigger物业的新扩展目标上完成的所有三个钻孔100%都与宽达135米的广泛硫化物矿化带相交*。所有三个洞的化验都在等待进行,一旦收到、编译和解释,就会公布。
- 这些重要的截获证实了在深部存在广泛的矿化系统,以及在各个方向保持开放的线性、广泛的矿化体的高潜力。
- 在位于下伏火山岩中的新延伸靶区观察到的矿化类型(包括半块状至块状磁黄铁矿和黄铁矿)、结构(包括脉状、网状和角砾化)和蚀变(绿泥化、硅化、绿帘化)与在上述沉积物中较高的Surebet带的钻孔和地表观察到的相似,强烈表明成矿流体的广泛下伏来源相同。
- 在新延伸目标的J垫上的GD-22-25钻孔与多个广泛的浸染性和脉状/角砾岩赋存的硫化物矿化相交,该矿化宽达95.5米*,在黑兹尔顿火山岩中含有磁黄铁矿、黄铁矿和黄铜矿。
- 位于新延伸目标的钻头J上的钻孔GD-22-26穿过一个宽阔的区域*,其中包含135米宽*的脉状/角砾岩容矿和浸染硫化物矿化,从基岩(30米)到孔底(165米),由磁黄铁矿(高达3%)、黄铜矿(高达1%)和黄铁矿(高达5%)组成。这个洞终止于硫化物矿化,并保持敞开。
- 这一公告附带的照片可在以下网址查阅
- 在新延伸目标的J垫上的GD-22-27钻孔穿过一个宽阔的区域,从基岩(57米)到165米,包含108米宽*的硫化物脉状和角砾岩,由磁黄铁矿(总体5%,局部块状厘米宽的切片),黄铁矿(1%,局部高达3%)和黄铜矿(微量,浸染)组成,并保持开放状态。
- 这一公告附带的照片可在以下网址查阅
- 广泛的成矿系统已被证实,沿Surebet区南北方向超过1公里,从Real Deal到位于新延伸目标的新钻探的Pad J东西方向2公里,该延伸目标仍然四通八达;见下图。
- Pad J的钻机将被移到Pad 15,向西1.6公里(Real Deal以南820米),以确定Surebet系统的深度,而第二次钻探将开始测试该系统在Hazelton火山岩中向北延伸到New Gold,Pad J以北2.5公里(北瓦砾以北1公里);见下图。
- 今年24,000米的计划钻探计划旨在从2021年起全方位扩大已知矿化范围,包括向西(至莱德湖,Real Deal西南940米),向北(至New Gold,北碎石以北1公里)和向东(至新延伸目标内的Pad J,Surebet东南1.5公里,面积5.25平方公里)。初步钻探已确认多个广泛矿化带的露头);见下图。
- 2022年的钻探计划将重点扩大Surebet高品位金银发现的已知参数,计划使用4个钻机在24个垫地位置的84个孔中钻探24,000米。它是为资源级加密钻探而设计的,并勾勒出东西长2.1公里,南北长2.5公里(5.25平方公里)的大型矿化系统。
- 这一公告附带的照片可在以下网址查阅
多伦多,2022年6月28日(环球通讯社)--Goliath Resources Limited(多伦多证券交易所股票代码:GOT)(OTCQB:GOTRF)(FSE:B4IF)(“公司”或《歌利亚》)很高兴地报告从其在Surebet发现的Surebet发现的延伸目标上的J Pad位置完成的钻探观察到其100%控制的Golddigger物业(The“财产”),不列颠哥伦比亚省金三角。到目前为止,在新延伸目标上完成的所有三个钻孔都返回了长达135米*的大量硫化物矿化区间。它们由脉状、网状和角砾岩中的半块状至块状磁黄铁矿、黄铜矿和黄铁矿组成的串状和集合体组成。在整个钻孔中观察到硫化物矿化作用,并保持开放状态。
在位于下伏火山岩中的新延伸靶区观察到的矿化类型(包括半块状至块状磁黄铁矿和黄铁矿)、结构(包括脉状、网状和角砾化)和蚀变(绿泥化、硅化、绿帘化)与在上述沉积物中较高的Surebet带的钻孔和地表观察到的相似,强烈表明成矿流体的广泛下伏来源相同。新延伸靶区的矿化赋存于黑兹尔顿火山岩(强烈蚀变的斜长-千粒状安山岩)和安山岩内的脉状/角砾岩中。相比之下,Surebet带的矿化主要赋存于切割黑兹尔顿沉积物的剪切带中。由于寄主岩石组成(特别是沉积物中的钙、镁含量低于安山岩)和岩石能力的不同,不同的寄主岩石之间的蚀变类型和发育的构造也不同,尽管它们可能是同一系统的一部分。
GD-22-26(方位角040°;倾角-55°)和GD-22-27(方位角150°;倾角-55°)是从2022年计划在延伸目标中最东侧的垫层Pad J上翻领的,位于露头Surebet东南1.5公里,Real Deal以东2公里处;见上图。
GD-22-26钻孔
GD-22-26钻孔(E 458908.947,N 6161976.043,方位角0 40°;倾角-55°)从基岩(30m)到井底(165m)截留硫化物矿化安山岩135m*。矿化主要以毫米至厘米大小的硫化物串状和集合体的形式出现在石英和石英-绿泥石-绿帘石脉体和角砾岩中,贯穿于强烈的绿帘化安山岩主岩中,并以弥漫在安山岩中的颗粒形式出现。大多数矿化由磁黄铁矿(总体3%,局部块状厘米宽的切片)、黄铁矿(3%,局部高达5%)和黄铜矿(集合体)组成。磁黄铁矿在整个孔洞中很常见,它以串状和集合体的形式出现在高度硅化的区域中,这些区域也含有绿泥石和绿帘石,并散布在主岩中。在84.79m和134.78米处,观察到了宽达2厘米的半块状到块状磁黄铁矿的角砾状剖面。黄铜矿聚集体在石英脉/角砾岩域中更为常见,通常延伸到
这个洞的最后10米含有不到2%的硫化物。然而,丰富的石英-绿泥石脉状和绿帘石蚀变一直持续到孔底,表明矿化仍向深部开放。
该洞以地表矿化为目标,包括一个渠道切割,在0.33米范围内分析6.7gpt Au,并抓取高达4.78gpt Au的样品。地表样品由含半块至块状方铅矿、黄铜矿、磁黄铁矿和黄铁矿的石英角砾岩组成。
GD-22-27钻孔
钻孔GD-22-27(E 458908.947,N 6161976.043,方位150°;倾角-55°)截留了108m*的硫化物矿化,赋存于基岩(57m)至165m的强烈蚀变安山岩中。矿化呈串状、脉状,呈浸染状分布,主要由磁黄铁矿和黄铁矿组成,并有少量黄铜矿。与GD-22-26钻孔相似,矿化主要以毫米至厘米级的串状硫化物和硫化物聚集体的形式出现在石英和石英-绿泥石-绿帘石脉体和角砾岩中,遍及强烈绿帘化的安山质火山主岩,并以弥漫在安山岩中的颗粒形式出现。大多数矿化由磁黄铁矿(总体5%,局部块状厘米宽的切片)、黄铁矿(1%,局部高达3%)和黄铜矿(微量,浸染)组成。磁黄铁矿在整个孔洞中很常见,它以串状和集合体的形式出现在高度硅化的区域中,这些区域也含有绿泥石,并分散在主岩中。与GD-22-25和GD-22-26孔相比,GD-22-27孔中绿帘石蚀变安山岩中含有较高比例的浸染型磁黄铁矿和磁黄铁矿-绿泥石脉。在整个岩芯,矿化安山岩表现为斑片状绿帘石蚀变,通常与含有硫化物矿化和石英绿泥石的微脉和裂缝有关。在GD-22-27钻孔中,硫化物矿化强度在顶部附近较高,向下达150m。这些截距与迄今为止从Pad J钻出的所有孔上的类似截距相关联,表明在深处存在广泛的线状矿化体的高潜力;见上图。
钻孔GD-22-27以地表矿化为目标,包括一个超过0.58米、长13.5gpt Au的渠道切割,并抓取高达44.4gpt Au的样品。地表样品由含半块至块状方铅矿、黄铜矿、磁黄铁矿和黄铁矿的石英角砾岩组成。
2022年演练活动
Pad J的钻机将被移到Pad 15,向西1.6公里(Real Deal以南820米),以确定Surebet系统的深度,而第二次钻探将开始测试该系统在Hazelton火山岩中向北延伸到New Gold,Pad J以北2.5公里(北瓦砾以北1公里);见上图。
在2022年的钻探活动中,Goliath计划对Surebet矿化系统进行深度测试,覆盖范围广泛,西至莱德湖(Real Deal西南940米),北至New Gold(北瓦砾以北1公里),重点是划定东西2.1公里、南北2.5公里的矿化区;见上图。根据2021年钻探结果和2020年渠道样本结果生成的预测模型,计划在Real Deal以西600米处规划几个钻探地点,以瞄准Surebet矿化系统的深度。从被认为与Surebet带有关的Real Deal和Cloud 9次级构造中采集的多个地表通道、芯片和Grab样品返回了显著的金银价值,进一步证实了深部存在一个大型的富含金银的矿化系统。这些二级结构被解释为充当流体进入地表的管道。位于Surebet以北1公里处的新金矿区计划进行一系列钻探。与新延伸目标相似,该带包含400米以上的地表金矿化,保持开放状态,露头观察到约30米的含金角砾岩。新黄金区位于黑兹尔顿火山岩中,非常接近红线。在金三角内发现的大多数世界级矿藏赋存于黑兹尔顿火山岩中,位于下黑兹尔顿岩石和斯图希尼岩石之间不整合(也称为红线)几公里范围内。
Goliath Resources创始人兼首席执行官罗杰·罗斯穆斯表示:对扩展目标的钻探不断带来令人兴奋的结果有100%的孔相交明显的硫化物矿化间隔,重申了在Golddigger矿藏上存在一个大型矿化系统。Goliath期待着未来几周,因为24,000米的钻探计划取得进展,新的信息和数据可以更好地确定Surebet这一广泛矿化系统的范围。“
Golddigger属性
Golddigger地产100%控制,占地23,859公顷(59,646英亩或239平方公里),位于不列颠哥伦比亚省金三角内世界级地质环境的Eskay裂谷,距离拥有多个世界级矿藏的红线不到2公里。该房产位于不列颠哥伦比亚省斯图尔特东南30公里处的潮水上。
Surebet以一系列NW-SE向构造为特征,这些构造赋存于黑兹尔顿火山之下的哈泽尔顿群沉积物中,距离红线不到几公里。2021年完成的所有24个钻石钻孔都与Au-Ag多金属矿化的重要区间相交,走向超过1公里,向下倾斜1.1公里,垂直起伏600米。钻孔GD-21-03*与6.37gpt AuEq(4.46gpt Au和122.13 gpt Ag)相交超过35.72米,而GD-21-05*钻孔与12.6gpt AuEq(8.06gpt Au和313.66 gpt Ag)相交超过6.38米。所有24个孔的平均品位和宽度分别为6.29gpt AuEq(4.35gpt Au和104.94 gpt Ag)。
激光雷达图像、无人机图像和现场观察已经在4平方公里的区域内发现了几个额外的平行结构。地球化学分析证实,这些构造中存在高品位的金银多金属矿化。陡峭倾斜的Real Deal和Cloud 9构造,以及来自延伸带的副射构造,显示出与Surebet带相似的矿化、地球化学和结构。地表和钻芯内的地质观察表明,Surebet带沿其较浅的倾斜几何结构,构造应变集中。Real Deal和Cloud 9被认为是与Surebet深度相连的梯队结构。矿化的Surebet带仍向四面八方开放。
有资格的人
Rein Turna P.Geo是国家仪器43-101定义的Goliath资源有限项目的合格人员,并监督本新闻稿中技术信息的准备,并已进行审查和批准。
其他
在不列颠哥伦比亚省泰瑞斯的MSALABS实验室,所有的岩石、水道和距骨细小样品都被粉碎和粉碎。MSALABS在其所有地点都通过了ISO9001:2008认证或ISO 17025:2005认证。在不列颠哥伦比亚省兰利市,用火试纸法和金属屏火法对所得样品纸浆中的金进行了分析。这些牙髓也在不列颠哥伦比亚省兰利的MSALABS实验室用多元素王水消化法进行了检测。粗略的岩石样本和纸浆一起被运往哥利亚资源有限公司位于不列颠哥伦比亚省泰瑞斯的储存设施。所有样品均采用MSALABS的分析程序ICP-130、1:1:1王水消解-电感耦合等离子体原子发射光谱分析(ICP-AES)或电感耦合等离子体质谱(ICP-MS)分析,以及Fas-121铅收集火焰分析结合原子吸收光谱分析(AAS)分析程序。任何超过100ppm的银或10000ppm的铜、铅和锌的结果都使用MSALABS针对每种元素的ICA-6xx方法进行额外检测。该方法采用硝酸-盐酸消解,然后进行电感耦合等离子体发射光谱分析(或滴定和重量分析)。金值大于10ppm的金是用Fas-425方法测定的,该方法包括重量分析熔融程序。另外,用MSALABS的MSC-150或MSC-350方法对Au大于5ppm的样品进行金属屏蔽火分析。将包括空白、标准和重复样品的QA/QC样品定期插入到样品序列中。
读者需要注意的是,抓取样本是典型的、但不完全限于矿化的斑点样本。GRAB样品是选择性的,收集的目的是确定矿化的存在或不存在,并不是为了代表所采样的材料。
关于歌利亚资源有限公司
Goliath Resources Limited是一家贵金属项目勘探商,位于不列颠哥伦比亚省西北部多产的金三角和魁北克省Abitibi Greenstone带。它的所有项目都位于世界级的地质环境和地缘政治安全管辖区,适合在加拿大进行采矿。
如需更多信息,请联系:
歌利亚资源有限公司
罗杰·罗斯穆斯先生
创始人兼首席执行官
电话:+1-416-488-2887 x222
邮箱:roger@goliathresource ces.com
* 宽度是以钻芯长度报告的,真实宽度是未知的,AUEQ金属价值的计算方法为: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。基于Goliath项目所在同一金三角矿营的其他采矿和勘探项目,如Homestake Ridge金矿项目(Auryn Resources技术报告、最新矿产资源估计和Homestake Ridge金矿项目的初步经济评估),从这些矿石中经济回收金、银、铜、铅和锌的潜力很大。在这里,AuEq值是使用金属价格的三年运行平均值计算的,其中包括冶金回收、处理费用、精炼成本和运输拨备。金、银、铜、铅的回收率分别为85.5%、74.6%、74.6%、45.3%。假设锌与铜的回收率相同,为74.6%。所引用的冶金回收不是来自Goliath的Golddigger项目,Surebet带矿化,也不能保证永远会实现这样的回收,除非最终能够完成Golddigger项目的详细冶金工作,如可行性研究中的工作。
多伦多证券交易所及其监管服务提供商(该术语在多伦多证券交易所的政策中定义)和OTCQB风险市场均不对本新闻稿的充分性或准确性承担责任。
本新闻稿中包含的某些陈述属于前瞻性信息。这些陈述与未来的事件或未来的表现有关。使用“可能”、“打算”、“预期”、“相信”、“将会”、“预计”、“估计”以及与非历史事实有关的类似表述和陈述,意在识别前瞻性信息,并基于歌利亚目前对此类未来事件的结果和时机的信念或假设。未来的实际结果可能会有很大不同。特别是,本新闻稿包含与公司完成融资的能力以及在开发其采矿资产时为股东创造价值的能力等相关的前瞻性信息。在得出结论或作出前瞻性信息中列出的预测或预测时,通常会应用各种假设或因素。这些假设和因素是基于歌利亚目前掌握的信息。虽然该等陈述是基于管理层的合理假设,但不能保证建议的交易将会发生,或如果建议的交易确实发生,将按上述条款完成。
本新闻稿中包含的前瞻性信息是截至本文发布之日的,除非适用的证券法要求,否则歌利亚没有义务因新信息、未来事件或其他原因而更新或修改任何前瞻性信息。由于本文包含的风险、不确定性和假设,投资者不应过度依赖前瞻性信息。上述陈述明确表示,本文中包含的任何前瞻性信息都是合格的。
本公告不构成认购或购买任何证券的要约、邀请或推荐,本公告或其中包含的任何内容均不构成任何合同或承诺的基础。特别是,本公告不构成在美国或任何其他司法管辖区出售或邀请购买证券的要约,在这些司法管辖区,此类要约是非法的。
本文提及的证券尚未、也不会根据修订后的1933年美国证券法(“美国证券法”)或任何州证券法进行注册,且不得在美国境内或为美国个人的账户或利益(如美国证券法下的S规则所定义)提供或出售,除非根据美国证券法和适用的州证券法注册,或获得此类注册豁免。
不得在美国传播或分发给美国新闻通讯社服务,也不构成本文所述证券的要约。
moomoo是Moomoo Technologies Inc.公司提供的金融信息和交易应用程序。
在美国,moomoo上的投资产品和服务由Moomoo Financial Inc.提供,一家受美国证券交易委员会(SEC)监管的持牌主体。 Moomoo Financial Inc.是金融业监管局(FINRA)和证券投资者保护公司(SIPC)的成员。
在新加坡,moomoo上的投资产品和服务是通过Moomoo Financial Singapore Pte. Ltd.提供,该公司受新加坡金融管理局(MAS)监管(牌照号码︰CMS101000) ,持有资本市场服务牌照 (CMS) ,持有财务顾问豁免(Exempt Financial Adviser)资质。本内容未经新加坡金融管理局的审查。
在澳大利亚,moomoo上的金融产品和服务是通过Futu Securities (Australia) Ltd提供,该公司是受澳大利亚证券和投资委员会(ASIC)监管的澳大利亚金融服务许可机构(AFSL No. 224663)。请阅读并理解我们的《金融服务指南》、《条款与条件》、《隐私政策》和其他披露文件,这些文件可在我们的网站 https://www.moomoo.com/au中获取。
在加拿大,通过moomoo应用提供的仅限订单执行的券商服务由Moomoo Financial Canada Inc.提供,并受加拿大投资监管机构(CIRO)监管。
在马来西亚,moomoo上的投资产品和服务是通过Moomoo Securities Malaysia Sdn. Bhd. 提供,该公司受马来西亚证券监督委员会(SC)监管(牌照号码︰eCMSL/A0397/2024) ,持有资本市场服务牌照 (CMSL) 。本内容未经马来西亚证券监督委员会的审查。
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.是关联公司。
风险及免责提示
moomoo是Moomoo Technologies Inc.公司提供的金融信息和交易应用程序。
在美国,moomoo上的投资产品和服务由Moomoo Financial Inc.提供,一家受美国证券交易委员会(SEC)监管的持牌主体。 Moomoo Financial Inc.是金融业监管局(FINRA)和证券投资者保护公司(SIPC)的成员。
在新加坡,moomoo上的投资产品和服务是通过Moomoo Financial Singapore Pte. Ltd.提供,该公司受新加坡金融管理局(MAS)监管(牌照号码︰CMS101000) ,持有资本市场服务牌照 (CMS) ,持有财务顾问豁免(Exempt Financial Adviser)资质。本内容未经新加坡金融管理局的审查。
在澳大利亚,moomoo上的金融产品和服务是通过Futu Securities (Australia) Ltd提供,该公司是受澳大利亚证券和投资委员会(ASIC)监管的澳大利亚金融服务许可机构(AFSL No. 224663)。请阅读并理解我们的《金融服务指南》、《条款与条件》、《隐私政策》和其他披露文件,这些文件可在我们的网站 https://www.moomoo.com/au中获取。
在加拿大,通过moomoo应用提供的仅限订单执行的券商服务由Moomoo Financial Canada Inc.提供,并受加拿大投资监管机构(CIRO)监管。
在马来西亚,moomoo上的投资产品和服务是通过Moomoo Securities Malaysia Sdn. Bhd. 提供,该公司受马来西亚证券监督委员会(SC)监管(牌照号码︰eCMSL/A0397/2024) ,持有资本市场服务牌照 (CMSL) 。本内容未经马来西亚证券监督委员会的审查。
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.是关联公司。
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