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Terra Balcanica Resources Continues Testing Brezani Porphyry Target In Bosnia And Closes Third Tranche Of Financing
Vancouver, British Columbia, July 20, 2023 (GLOBE NEWSWIRE) -- Terra Balcanica Resources Corp. (“Terra” or the “Company”) (CSE:TERA; FRA:UB1) is pleased to anno
About this update from Terra Balcanica Resources Corp.
[{"type":"text","content":" Vancouver, British Columbia, July 20, 2023 (GLOBE NEWSWIRE) -- Terra Balcanica Resources Corp. (“Terra” or the “Company”) (CSE:TERA; FRA:UB1) is pleased to announce closing of the 3rd tranche of the non-brokered private placement financing (the “Offering”) of units (the ”Units”) as it continues drilling the Brezani porphyry target in eastern Bosnia and Herzegovina. Brezani Phase II Drilling Campaign The Company is testing a 650 m wide conductivity high at the centre of an anomalously magnetic volume of rock, 1.2 km in diameter, where potassic altered porphyritic andesites overprinted by chlorite are found below a gold-bearing skarn (Figure 1). Here, the electrically resistive unit returned 88.0 m of 0.61 g/t AuEq from surface (see Company news release dated 24th of January 2023). The redrilled Phase I drill hole has now been extended beyond its 2022 terminal depth of 215 m along the same dip and azimuth. The HQ diameter diamond drill bit has now reached 468 m as it progresses at a rate of ca. 20 m daily to intercept the >60 mS/m conductor in a week. Figure 1. A NW-SE geophysical cross section showing the trajectory of the drillhole BREDD002. At 323m, the conductivity reaches 15mS/m and coincides with a pyrite rich footwall indicating that the subsurface resistivity is chiefly controlled by the rock sulfide content. Phyllic altered feldspar phyric andesite (lower right) contains marcasite rich groundmass with up to 2,000 ppm Sb and 600 ppm Co. Also present are pyrite veins with crosscutting calcite centrelines that yield up to 1,000 ppm Cu (click here to view image). BREDD002 Geology From 240 m to 374.7m below surface, Terra’s BREDD002 drillhole has intersected a large package of phyllic altered hornfels with intermittent porphyry intrusions, crosscut at high angles and associated with both calc-silicate alteration and carbonate base metal veining. At depth of 320 m and spatially coincident with a sub-horizontal conductivity change drilling has penetrated an intensely silicified structure underneath which there is a substantial increase in the volume of sulfide minerals and density of carbonate base metal veins (Figure 2). This structure, interpreted as a low-angle reverse fault, appears to intersect surface toward NW around the same area where gossanous material was previously mapped. It is suggested that this zone could be ...