AMERICA

America is located 85 km SSE from Copiapo and comprises 8.200 hectares of exploration claims.

Geology

Locally composed of volcanic andesite , dacite , tuff ), intruded by multiple intrusives (68 to 62 ma. U/Pb), porphyries (61,7 61,9 ma. U/Pb) and hydrothermal igneous breccias.
Overprinted by chlorite epidote halo, silica quartz clay sericite , tourmaline alteration.
Mineralization composed of jarosite goethite hematite , Ox. Cu traces. Distributed in stockwork veinlets and disseminate.
Hydrothermal system controlled by NW and NE fault breccias veins system

Drilling

A pyritic propylitic halo drilled

GEOLOGY

Cu-Mo Porphyry

Regionally located on the Honitos Formation (volcano sedimentary rocks), intruded by El Carrizo pluton (upper cretaceous sup. to lower palecene belt).
The southern edge of America extends to the Relincho paleocene deposit, with 1BT @ 0.5% CuEq (Mo).

Local Geology

Locally composed of volcanic andesite , dacite , tuff ), intruded by multiple intrusives (68 to 62 ma. U/Pb), porphyries (61,7 61,9 ma. U/Pb) and hydrothermal igneous breccias.
Overprinted by chlorite epidote halo, silica quartz clay sericite , tourmaline alteration.
Mineralization composed of jarosite goethite hematite, Ox. Cu traces. Distributed in veins and disseminate.
Hydrothermal system controlled by NW and NE fault breccias veins system.
Quartz veinlets system open to South East.

250m x 250m sampling grid; 251 samples (4 Acid Digestion + 48 elements by ICP + Au by Fire assay); Coverage area (1500 ha)

DRILLING

3.907,1 m. distributed in 9 drilholes (DDH), to confirm a hydrothermal system type porphyry (Cu Mo). The drilled zone is most quartz sericite environment. The target zone is open below 400m. depth, and fully open in SE direction .

The América porphyry system, is composed by multiple intrusive, porphyry, igneous and hydrothermal breccias events.
Early biotite-chlorite-Fk-Ep-Mag, overprinted by chlorite-sericite-biotite, sericite-qz-chlorite, clays-sericite alterations.
Almost 4 main mineralization events have been identified at date (early magnetite; very early molibdenite; early molibdenite-calcopirite-pirite, and pirite-calcopirite events).