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Luminex Discovers a New Porphyry Copper Target at Cascas

Luminex Discovers a New Porphyry Copper Target at Cascas

Luminex在卡斯卡斯發現新的斑巖銅靶
PR Newswire ·  2021/09/24 07:10

Highlights:

重點:

  • The Hapa "Bullseye" target is a 1 km diameter coincident soil copper/molybdenum anomaly
  • Part of a trend of porphyry copper systems discovered in western Cascas
  • Rock chip and channel samples assaying as high as 1.29% copper and 0.33% molybdenum
  • HAPA的“鬥牛眼”目標是直徑1公里的重合土壤銅/鉬異常。
  • 喀斯喀斯西部發現斑巖銅礦系統趨勢的一部分
  • 巖屑和孔道樣品分析高達1.29%的銅和0.33%的鉬

VANCOUVER, BC, Sept. 24, 2021 /PRNewswire/ - Luminex Resources Corp. (TSXV: LR) (OTCQX: LUMIF) (the "Company" or "Luminex") is pleased to announce the discovery of a new porphyry copper target: Hapa, located in the northwestern part of the Company's 100% owned Cascas property. Hapa and Shakai lie on a northwest-southeast trending ZTEM feature that could be a district feature controlling emplacement. The Hapa target is situated 3 km to the northwest of the Shakai porphyry copper centre and was first recognized by company geologists while executing a 200m x 300m grid soil sample survey. The soil grid, orientated northwest-southeast, follows the 2019 ZTEM geophysical survey lines (Figure 1).

公元前温哥華,9月2021年2月24日/美通社/-Luminex Resources Corp.納斯達克股票代碼:LUMIF)(多倫多證券交易所股票代碼:LUMIF)(“本公司”或“Luminex”)高興地宣佈發現一個新的斑巖銅礦目標:Hapa,位於公司全資擁有的Cascas礦產的西北部。Hapa和Shakai位於西北-東南方向的ZTEM特徵上,這可能是控制侵位的區域特徵。Hapa目標位於沙開斑巖銅礦中心西北3公里處,公司地質學家在執行200米x300m網格化土壤抽樣調查。土壤網格為西北-東南方向,遵循2019年ZTEM地球物理測量線(圖1)。

Figure 1. Location map of Hapa showing Cascas soil sample grids, major faults and ZTEM geophysics (CNW Group/Luminex Resources Corp.)
圖1.顯示Cascas土壤樣本網格、主要斷層和ZTEM地球物理的HAPA位置圖(CNW集團/Luminex Resources Corp.)
Figure 2. Soil sample locations with contoured copper and molybdenum and rock chip sample results for those returning >0.3% copper. (CNW Group/Luminex Resources Corp.)
圖2.帶等高線銅、鉬和巖屑樣品的土壤樣品位置,對於那些銅含量>0.3%的樣品,其結果是。(CNW集團/Luminex Resources Corp.)
Figure 3. Hapa rock samples and mineralization styles. (CNW Group/Luminex Resources Corp.)
圖3。哈帕巖樣和礦化類型。(CNW集團/Luminex Resources Corp.)
Figure 4. Geology of the Hapa target with superimposed soil copper geochemistry. (CNW Group/Luminex Resources Corp.)
圖4.疊加土壤銅地球化學的HAPA靶區地質(CNW集團/Luminex Resources Corp.)
Figure 5. Schematic geological cross section (upper) and comparable surface view (lower). (CNW Group/Luminex Resources Corp.)
圖5.示意圖地質剖面圖(上)和可比表面圖(下)。(CNW集團/Luminex Resources Corp.)

Figure 1. Location map of Hapa showing Cascas soil sample grids, major faults and ZTEM geophysics

圖1.顯示Cascas土壤樣本網格、主要斷層和ZTEM地球物理的HAPA位置圖

Subsequent to its discovery, the size and shape of the Hapa target was defined by infill soil sampling on a 100m x 100m grid within the anomalous area (Figure 2). To date, rock chip and channel samples along creeks have assayed as high as 1.29% copper and 0.33% molybdenum. Copper and molybdenum mineralization occurs as disseminations and blebs in granodiorites, as porphyry-style quartz vein sets and as banded sulphide-rich veins comprising pyrite, chalcopyrite, chalcocite, covellite and molybdenite (Figure 3). Native sulphur has also been noted in outcrop and an elevated soil sulphur anomaly coincides with copper, molybdenum and tungsten anomalies in that soil survey data, all indicative of porphyry mineralization. The copper and molybdenum anomaly forms an irregular "bullseye" with a diameter of approximately 1,000m when contoured at the 400 ppm copper and 20 ppm molybdenum levels. The host rocks are hydrothermally altered and locally faulted granodiorite, granodiorite porphyry and diorite magmas of the Zamora batholith. Late, localized porphyry dikes cut intrusive rocks.

在它被發現之後,hapa目標的大小和形狀是由100m x的填充土壤取樣確定的。100m異常區域內的網格(圖2)。到目前為止,沿小溪的巖屑和渠道樣品已檢測到高達1.29%的銅和0.33%的鉬。銅和鉬礦化在花崗閃長巖中以浸染和氣泡的形式出現,以斑巖型石英脈組和由黃鐵礦、黃銅礦、輝銅礦、斜輝石和輝鉬礦組成的條帶狀富硫化物礦脈的形式出現(圖3)。在露頭中也發現了自然硫,土壤硫異常升高與該土壤調查數據中的銅、鉬、鎢異常相吻合,均指示斑巖成礦。銅鉬異常在400ppm銅和20ppm鉬水平等高時形成直徑約1000米的不規則“靶眼”。容礦巖石為熱液蝕變局部斷裂的花崗閃長巖、花崗閃長斑巖和閃長巖漿。薩莫拉巖基。晚期,局部斑巖巖脈切割侵入巖。

Figure 2. Soil sample locations with contoured copper and molybdenum and rock chip sample results for those returning >0.3% copper.

圖2.帶等高線銅、鉬和巖屑樣品的土壤樣品位置,對於那些銅含量>0.3%的樣品,其結果是。

Figure 3. Hapa rock samples and mineralization styles.

圖3。哈帕巖樣和礦化類型。

Geological mapping along creeks at Hapa has delineated an elliptical zone of sericite-quartz (phyllic) alteration, approximately 1 km in diameter which coincides with the soil copper and molybdenum anomalies. Close to the centre of the phyllic zone is a narrow window of potassic alteration (potassium feldspar (Figures 4 and 5). Outboard of the phyllic zone, the hydrothermal alteration changes to propylitic, characterized by a chlorite-epidote-carbonate-magnetite mineral assemblage. This concentric zonation of hydrothermal alteration minerals is typical of copper porphyry deposits.

沿哈帕小溪填圖,圈定了直徑約1公里的絹雲母-石英(葉狀)蝕變橢圓形帶,與土壤銅、鉬異常相吻合。靠近葉狀帶中心的是一個狹窄的鉀質蝕變窗口(鉀長石)(圖4和圖5)。葉狀帶外側,熱液蝕變為綠泥石,以綠泥石-綠簾石-碳酸鹽-磁鐵礦礦物組合為特徵。這種熱液蝕變礦物的同心分帶是典型的銅斑巖礦牀。

Figure 4. Geology of the Hapa target with superimposed soil copper geochemistry.

圖4.疊加土壤銅地球化學的HAPA靶區地質

Luminex interprets that a porphyry copper intrusion is located underneath the geochemically anomalous area of Hapa indicating good preservation of the phyllic and underlying potassic alteration zones and the potential for secondary copper enrichment. The target area centres on a rugged hill, possibly the product of differential uplift between two formative faults that facilitated emplacement of the porphyry system (see Figure 5).

Luminex解釋説,斑巖銅巖體位於Hapa地球化學異常區域之下,表明葉狀和下伏鉀質蝕變帶保存良好,並具有次生銅富集的潛力。目標區域集中在一座崎嶇的山丘上,可能是兩條形成斷層之間差異隆升的產物,這兩條斷層促進了斑巖系統的就位(見圖5)。

Figure 5. Schematic geological cross section (upper) and comparable surface view (lower).

圖5.示意圖地質剖面圖(上)和可比表面圖(下)。

Qualified Persons

合格人員

Leo Hathaway, P. Geo, Senior Vice President Exploration of Luminex and the Qualified Person as defined by National Instrument 43-101 Standards of Disclosure for Mineral Projects, has reviewed, verified and approved the scientific and technical information in this news release and has verified the data underlying that scientific and technical information.

Leo Hathaway,P.Geo,Luminex勘探高級副總裁和National Instrument 43-101定義的合格人員礦產項目信息披露標準已經審核、核實和批准了本新聞稿中的科學技術信息,並核實了該科學技術信息背後的數據。

About Luminex Resources

關於Luminex資源

Luminex Resources Corp. (TSXV:LR,OTCQX:LUMIF) is a Vancouver, Canada based precious and base metals exploration and development company focused on gold and copper projects in Ecuador. Luminex's inferred and indicated mineral resources are located at the Condor Gold-Copper project in Zamora-Chinchipe Province, southeast Ecuador. Luminex also holds a large and highly prospective land package in Ecuador, including the Tarqui and Pegasus projects, which are being co-developed with BHP Group plc and Anglo American respectively.

Luminex Resources Corp.(多倫多證券交易所股票代碼:LR,OTCQX:LUMIF)是一家總部位於加拿大温哥華的貴金屬和賤金屬勘探開發公司,專注於加拿大温哥華的金礦和銅礦項目。厄瓜多爾。Luminex推斷和指示的礦產資源位於厄瓜多爾東南部薩莫拉-欽奇佩省的禿鷹金銅項目。Luminex還持有一個大型且極具前景的土地組合厄瓜多爾包括分別與必和必拓集團(BHP Group Plc)和英美資源集團(Anglo American)共同開發的Tarqui和Pegasus項目。

Further details are available on the Company's website at https://luminexresources.com/.

欲瞭解更多詳情,請訪問公司網站:https://luminexresources.com/.。

To receive news releases please sign up at https://www.luminexresources.com/contact/contact-us/.

要接收新聞發佈,請在https://www.luminexresources.com/contact/contact-us/.上註冊

LUMINEX RESOURCES CORP.

Luminex Resources Corp.

Signed: "Marshall Koval"

簽署:“馬歇爾·科瓦爾”

Marshall Koval, CEO and Director

馬歇爾·科瓦爾, 首席執行官兼董事

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

多倫多證券交易所創業板交易所及其監管服務提供商(該術語在多倫多證券交易所創業板政策中定義)均不對本新聞稿的充分性或準確性承擔責任。

SOURCE Luminex Resources Corp.

來源:Luminex Resources Corp.

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