The San Antonio project is located 70 km south of Medellin and 8 km NNE of the Guayabales project on the western margin of the Colombian Central Cordillera. The project incorporates porphyry Cu-Au-Mo mineralization and associated hydrothermal alteration over an area of 2 km x 1 km. This area locates immediately adjacent to the regional Romeral Fault system. The Miocene aged, mineralized porphyry intrusives are hosted in Paleozoic schists and Cretaceous age mafic volcanic rocks. Porphyry mineralization is exposed over large areas as both sheeted and stockwork vein systems and breccias associated with a multi-kilometer scale Au-Mo-Cu soil anomalies and associated hydrothermal alteration. Previous operators of the project did not drill the main porphyry occurrences and were targeting high-grade vein style mineralization locating peripheral to the porphyry intrusive centers