The Josnitoro Gold Project is located approximately 600 kilometres by road southeast of Lima in the Department of Apurimac, southern Peru. There are no communities or families living on the mining concession area. Two communities, approximately 50 km distance, own the surface rights.
Historical work on the project has consisted of geologic mapping and rock chip and trench sampling. Past rock chip samples on the property have returned results of up to 7.74 g/t Au, and trench sampling has returned results of up to 33.6 g/t Au.
There have been 174 rotary percussion holes drilled on the property up to 18m deep each for a total drill amount of 2,856m. Highlights include 12m @ 4.02 g/t Au and 6m @ 4.88 g/t Au.
The mineralization at Josnitoro has been recognized in two styles (and areas):
- The Cu-Au skarn mineralization related to the Ferrobamba calcareous formation and associated with the diorite intrusion, which presents the typical garnet-wollastonite-barite-sericite-magnetite-specularite assemblage, with economic Cu-Zn-Pb sulfides contents and important premium in Au. This mineralization is located in the Huancabamba Community lands.
- The gold dissemination within the quartzite and sandstones of the Soraya formation is marked by Au-As-Pb-Cu-Zn anomalies at surface. This sequence is crosscut by hydrothermal sub-vertical breccias that have been altered showing the following assemblage: illite, smectite, kaolin, goethite, quartz, jarosite, scorodite, goethite and hematite. Gold mineralization is primarily controlled by the local structures and it is also disseminated in the fractured sandstones and quartzites.