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Palladium One, Kaukua South Chargeability Anomaly Expanded to Over Four Kms at LK PGE-Ni-Cu Project in Finland
Vancouver, British Columbia--(Newsfile Corp. - April 14, 2020) -   Palladium One Mining I...
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[{"type":"text","content":"Palladium One, Kaukua South Chargeability Anomaly Expanded to Over Four Kms at LK PGE-Ni-Cu Project in FinlandVancouver, British Columbia--(Newsfile Corp. - April 14, 2020) -  Palladium One Mining Inc. (TSXV: PDM) (FSE: 7N11) (OTC Pink: NKORF) (the \"Company\" or \"Palladium One\") is very pleased to report that the Kaukua South Zone anomaly extends over more than a four (4) km strike length and into a large overburdened area that has never been drill tested. Final results from the first Induced Polarization (IP) survey grid, Kaukua East and the Infill grid (see news release February 25, 2020) have outlined this large chargeability anomaly, representing the eastern extension of the palladium dominant Kaukua South Zone. (Figure 1, 2 and 3)The Kaukua South anomaly extends to the eastern edge of Kaukua East IP survey grid, and the edge of the Exploration Permit boundary. As a result, the Company has applied for a 9,100-hectare Reservation (Kaukuanjarvi), (see press release April 2, 2020) covering the potential extension of the Kaukua South zone (Figure 4). A review of regional airborne geophysics indicates an east-west magnetic trend beyond the currently mapped extent of the Kaukua area mafic-ultramafic rocks, could be an extension of the Kaukua South mineralization. Reservations are granted for 1-2 years and have no holding costs. Figure 1. Plan view of the 2008 and 2020 (current) IP survey in the Kaukua Area. The 2008 IP survey area is outlined in blue, while the 2020 survey is outlined in green. The Kaukua deposit's optimised open pit is outlined by a dashed black line (see details below). The newly expanded Kaukua South Zone south is outlined by a dashed orange line. The 2008 IP survey was instrumental in identifying the Kaukua Deposit. The 2008 survey used different equipment, consisting of a 3-line 3D system, whereas the 2020 survey used a 5-line 3D system, as a result the two surveys are not exactly comparable.To view an enhanced version of Figure 1, please visit:https://orders.newsfilecorp.com/files/6502/54374_50a88f57f4d0f897_001full.jpg Figure 2. Long section view, looking north, of the Kaukua deposit and the newly expanded Kaukua South Zone chargeability anomaly. To view an enhanced version of Figure 2, please visit:https://orders.newsfilecorp.com/files/6502/54374_50a88f57f4d0f897_002full.jpg Figure 3. Iso...