The four drillholes were located on the main lens, with the aim of characterizing the mineralization

present as well as the host rocks, in order to define a metallogenic model for further exploration. The

mineralization intersected in drillhole F08-01 consists primarily of veins and veinlets (stockwork) of

massive chalcopyrite located in a chloritized basalt, while drillhole F08-03 intersected 40 metres of

massive sulphide, mainly composed of pyrite, sphalerite, chalcopyrite, and magnetite. Moreover, the

host rocks observed in drillholes F08-02 and F08-04 consist mainly of basalt and andesite, confirming

that this is indeed a volcanogenic massive sulphide (VMS) deposit.

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