Asiamet Resources Limited announced that ongoing exploration drilling at the BKZ Polymetallic ("BKZ") prospect located on its Kalimantan Surya Kencana ("KSK") 6th Generation Contract of Work ("CoW"), in Central Kalimantan, Indonesia continues to intersect shallow, high grade base and precious metal rich mineralisation. Highlights to date include: BKZ deposit comprises high grade polymetallic Zn-Pb-Cu-Ag-Au mineralisation underlain by copper-silver mineralisation that is either massive sulphide or vein style. Mineralisation is confirmed over a strike length of 300m and up to 110m in width. Thickness is variably 5m to 40m. Five holes have now intersected the high grade copper-silver mineralisation that underlies the high grade polymetallic Zn-Pb-Cu-Ag-Au mineralisation, confirming at least 150m strike length and 50m in true thickness. Mineralisation remains open to the south, east, west and down-dip. New assays confirm further high grade copper-silver mineralisation within the interpreted "Feeder Structure" underlying the polymetallic mineralisation at BKZ, with up to 7.9% copper over 1-metre sample intervals. Drilling at BKZ has been upgraded to "Delineation Drilling Status comprising an estimated 3500m in 30 holes to provide sufficient drill data density in order to define a maiden Resource for the polymetallic mineralisation and the underlying copper-silver mineralisation at BKZ. Highlights of the latest batch of drill results received include: BKZ33550-01: 5.0m at 4.4% zinc, 1.6% lead, 46g/t silver and 0.11g/t gold (from 44.0m); 38.0m at 1.26% copper, 9g/t silver, 0.13g/t gold (from 49.0m); Including 3m at 1.59% copper, 14g/t silver, 0.22g/t gold (from 50.0m); Including 21m at 1.78% copper, 11g/t silver, 0.14g/t gold (from 65.0m); Includes 7m at 2.81% copper, 15g/t silver, 0.19g/t gold (from 65.0m); Includes 4m at 2.71% copper, 12g/t silver, 0.14g/t gold (from 74.0m). BKZ33500-01: 12.0m at 4.0% zinc, 1.7% lead, 9g/t silver and 0.10g/t gold (from 54.5m). To date, twenty holes (2133m metres in total) have been drilled to test the upper zone of polymetallic massive sulphide and vein style mineralisation and the lower zone of vein hosted copper - silver mineralisation. The first scout hole on section line BKZ33550 was drilled westward to confirm continuity of mineralisation between section lines BKM33600 and BKM33550, where hole BKZ33600-02 (89.6m End of Hole "EOH") intersected a broad zone of copper-silver mineralisation from 59m depth hosted in quartz-sulphide veins. Hole BKZ33550-01 (116.7m EOH) was collared 50m south-southeast of BKM33600-02 and intersected vein-style polymetallic mineralisation underlain by high grade copper mineralisation contained within a dense stockwork of quartz-sulphide and sulphide veins containing bornite, chalcopyrite and pyrite. The hole was terminated due to rock hardness and rig capacity, with the final 18.7m comprising strongly silicified and oxidised rock. Assays confirm the oxidised zone contains gold-silver mineralisation and the final 1.7m sample assayed 0.32g/t gold and 31g/t Ag. The first scout hole on section line BKZ33500 was drilled westward to confirm continuity of mineralisation intersected on section line BKM33550. Hole BKZ33500-01 (118.5m EOH) was collared 50m south-southeast of hole BKM33550-01 and intersected vein-style polymetallic mineralisation underlain by multiple zones of moderate grade copper mineralisation contained within a dense stockwork of quartz-sulphide and sulphide veins containing chalcopyrite and pyrite. The first scout hole on section line BKZ33450 was drilled westward to confirm continuity of mineralisation intersected on section line BKM33500. Hole BKZ33450-01 (151.5m EOH) was collared 50m south of hole BKM33500-01, but failed to intersect the significant zones of moderate to high grade copper mineralisation that were intersected in drill holes BKZ33500-01 and BKZ33550-01. Hole BKZ33450-01 intersected several microdiorite and diorite porphyry dykes, up to 25m in width. This is the first drill hole that intersected post mineral microdiorite and diorite porphyry dykes, hence a structural model is required as the mineralisation could be offset by post-mineral faults. This 3D structural and geologic modelling work is ongoing, and drilling will continue to enhance knowledge of the mineralised system at BKZ.