Winshear Gold Corp. reported its first sampling results from the Gaban Gold Project located in the Puno Orogenic Gold Belt (“POGB”) in south-eastern Peru. Winshear is conducting exploration to locate the hard-rock source of alluvial gold in the Yanamayo and Piquitiri rivers, which drain into the Madre de Dios basin. In 2018, a heli-borne geophysical survey was flown over Gaban as part of a systematic exploration program that outlined regional structures with the potential to host gold mineralization. To date five shear zones have been identified on the property. First field programme conducted by Winshear Gold focused on the Coritiri stream sediment anomaly. 81 channel samples of bedrock (1.0-2.5m in length) were collected; 17 samples returned 0.1g/t – 0.49 g/t Au; 6 samples returned 0.5 g/t – 0.99 g/t Au; 7 samples returned 1.0 g/t – 4.99 g/t Au; 2 samples returned 5.0 g/t – 9.99 g/t Au; and 1 sample assayed 15.75 g/t Au. Highlights include 15.75g/t Au over 1m, 5.72g/t Au over 1.5m, 3.57g/t Au over 2.5m, and 5.7g/t Au over 1m. The mineralized area correlates strongly with an east-southeast trending geophysical target that is open to the east southeast and west northwest. Samples were collected from sheared sedimentary rocks, typically siltstones and shales /slates, with varying amounts of quartz veining. The sediments are identified as belonging to the Ordovician San Jose Group. Quartz veins vary in thickness from 1mm up to 80cm in width. Up to 3% sulphides (pyrite and arsenopyrite) are associated with the quartz veins. The geology in the target area correlates well with other known deposits in the POGB including the Ollachea Project 40 km to the SW. Numerous old prospect adits were discovered in the area, some of which were up to 15m long.