Avrupa Minerals Ltd
OTC Pink - Current Information:AVPMFView on Canadian Exchange

  • LAST PRICE
    0.0164
  • TODAY'S CHANGE (%)
    0.0000 (0.0000%)
  • Bid / Lots
    0.0100/ 100
  • Ask / Lots
    0.1220/ 50
  • Open / Previous Close
    --- / 0.0164
  • Day Range
    ---
  • 52 Week Range
    0.0100
    0.9999
  • Volume
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  • Nov 27, 2024

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    • 4:16PM ET on Wednesday Nov 27, 2024 by Dow Jones
      Companies Mentioned: AVU

      November, 27, 2024 -- (Avrupa Minerals Ltd.) -- (TheNewswire)

      Vancouver, BC, November 27, 2024 -- TheNewswire - Avrupa Minerals Ltd. (TSXV: AVU) reports that first-pass scout drilling at the Company's Kangasjärvi project in central Finland has been completed. Avrupa, through the JV entity Akkerman Finland Oy ("AFOy" -- Akkerman Exploration b.v. 51%; Avrupa 49%), completed two holes in the Kangas Main EM target area, totaling 709.3 meters. A third hole, testing the Kangas North EM anomaly was postponed due to terrain access issues. AFOy noted that the two holes were aimed at an untested EM anomaly located directly north of the old Kangasjärvi workings, across a prominent fault. The first was drilled from west to east into the conductor, while the second approached the anomaly from the south. Both holes successfully intersected vein-type and semi-massive mineralization. The first hole KM-01, intersected intermittent sulfides over a length of 82 meters from 194 meters to 276 meters depth. AFOy also noted that intermittent mineralization in the second hole, KM-02, was more intense and present over a wider interval between 119 meters and 341 meters, down-hole. Pyrite and pyrrhotite are the main sulfide minerals present with local, small amounts of chalcopyrite and minor sphalerite. Mineralization is accompanied by intense hydrothermal alteration of the original mafic volcanic host rocks. The intercepts are characteristic of a stockwork feeder zone. The sulfide veins and semi-massive replacement mineralization, accompanied by silicification, white mica and cordierite, are directly comparable with the mineralization and alteration found in the footwall of the Pyhäsalmi massive sulfide deposit, located 30 km to the north.

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