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    Unigold Intersects 8.9 g/t Gold, 37.1 g/t Silver, 0.2 Percent Copper and 2.4 Percent Zinc over 7 Meters

    Charlotte McLeod
    Apr. 11, 2016 04:47PM PST
    Gold Investing

    Unigold Inc. (TSXV:UGD) announced results from exploration drilling at its Candelones Extension deposit, located at its Dominican Republic-based Neita concession.

    Unigold Inc. (TSXV:UGD) announced results from exploration drilling at its Candelones Extension deposit, located at its Dominican Republic-based Neita concession.
    As quoted in the press release:

    The Company has received results from five holes testing Target C (REF Figure 1.0), near the currently defined western limit of the Candelones Extension deposit. Historical holes LP52 (15.9 metres @ 11.36 g/t Au; 38.3 g/t Ag; 0.4% Cu; 5.1% Zn) and LP57 (10.0 metres @ 6.71 g/t Au; 2.0 g/t Ag; 0.1% Cu; 0.6% Zn), define a potential vertical feeder system (REF Figure 2.0). West of LP52, historical drilling intersected relatively flat lying mineralization, dominated by sphalerite and barite, localized at the andesite – dacite contact.
    LP16-103 targeted the midpoint between holes LP52 and LP57; intersecting 7.0 metres @ 8.86 g/t Au; 37.1 g/t Ag; 0.2% Cu and 2.4% Zn.
    LP16-104, 50 metres to the west, intersected 3.3 metres @ 5.06 g/t Au; 90.0 g/t Ag; 0.2% Cu and 2.1% Zn.
    LP16-105, 100 metres to the west, intersected 8.0 metres @ 6.30 g/t Au; 16.9 g/t Ag; 0.1% Cu and 0.9% Zn.
    The three holes also roughly bisect a 200 metre gap in the historical drill pattern between holes LP70 and LP54 (REF Figure 3.0), both of which failed to intersect any mineralization of note. West of LP70, historical hole collars shifted to the north, tracking the flat lying portion of the andesite – dacite contact. These latest results suggest that there may possibly be additional resource potential south of the historical drilling.
    The results suggest E-W metal zonation, represented by gold and copper rich, pyrite dominated massive sulphides in the east, changing to gold, zinc, silver mineralization associated with quartz – barite veining to the west. The results define a structural corridor that is 75 to 100 metres in vertical thickness, plunging at approximately 25-30° to the east from Target C through Target A and beyond (REF. Figure 4.0). This structural corridor contains the majority of the high grade results intersected at the Candelones Extension with the exception of some results at Target B, which are interpreted to be related to a vertical epithermal feeder system.

    Click here to read the full Unigold Inc. (TSXV:UGD) press release.

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