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Durango Identifies Additional Areas of Interest at Windfall Lake, QC
(TheNewswire) Vancouver, BC - TheNewswire - October 8, 2020 - Durango Resourc...
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[{"type":"text","content":"Durango Identifies Additional Areas of Interest at Windfall Lake, QC\n \n \n (TheNewswire)\n \n \n \n \n \n \n \n Vancouver, BC - TheNewswire - October\n8, 2020 - Durango Resources Inc.\n \n \n (TSXV:DGO) (Frankfurt-86A1) (OTC:ATOXF),\n \n \n (the\n\"\n \n \n Company\n \n \n \" or \"\n \n \n Durango\n \n \n \") is pleased to report that\nfurther to its news release dated September 11, 2020, mechanical\ntrenching has identified additional areas of interest on its Trove\nProperty at Windfall Lake,\n \n \n \n \n Quebec\n \n \n .\n \n \n \n \n \n \n \n \n Click Image To View Full Size\n \n \n \n \n Figure 1 - Mineralized contact volcanic-sediment with\ncarbonate alteration\n \n \n \n \n The new outcrops are located within 100 metres from the\nfirst series of planned drill holes on the Trove Property which are\ndesigned to test continuity of mineralized trend between two drill\nintersections of Osisko Mining Inc. (TSX-OSK) (\n \n \n OSK-UB-18-083 intersected 1.03 g/t Au and 5.13 g/t Au,\nOSK-UB-18-085 intersected 1.85 g/t Au) as well as\n \n \n near surface geophysical targets with coincident till with\ngold grains and gold anomalies in the rock samples. The new outcrop is\nin proximity of the northeast shear zone and is a contact zone of the\nvolcanics and sediments. Mineralization was observed in a felsic dike\nwith pyrite in quartz veining and carbonate alteration on the newly\nstripped outcrops.\n \n \n \n \n \n \n \n \n Click Image To View Full Size\n \n \n \n \n Figure 2 - Biotite-chlorite altered sediment with\nmineralized quartz carbonate vein\n \n \n \n \n Durango's technical team recently discovered a\nnortheast trending shear zone on the Trove Property as announced on\nSeptember 11, 2020. In the Windfall Lake deposit area, the volcanic\nrocks are intruded by a series of felsic dikes near contacts between\nvolcanic and sediments which host quartz veins with pyrite. The team\nhas also confirmed an important regional deformation northeast shear\nwith carbonate alteration in the wall rock zones that delineate the\nstructural domains.\n \n \n \n \n \n \n \n \n Click Image To View Full Size\n \n \n \n \n Figure 3 - Mineralized 3-5% fine disseminated pyrite\nfelsic dyke in volcanic near contact with sediment\n \n \n \n \n Additional mineralization was also seen in the nearby\nsediments represented by pyrite, pyrrhotite and molybd...