The Buldibuyo Project is located within the Pataz - Parcoy - Buldibuyo gold-bearing metallotect, at its southern end.
Runoff sediment samples collected along the streams in the study area were collected and recorded.
A second ground geophysics campaign was completed in October 2008. Magnetometry and induced polarization studies were applied.
The exploration activities and results obtained allowed detecting the existence of hydrothermal alteration of siliceous, phyllic and propylitic type.
