Tepal’s proposed pits (in white) line up within a jog of a regional NE structure.
Mineralization is hosted in rocks depleted in K.
Very little intrusion occurs on the property or in core. Host rock is a highly clay altered andesite breccia with little silica.
This was a strong indication that something more that a porphyry deposit may be underlying the property.
Importantly, it has a regional scale exploration potential.