Central Vein fluid Inclusions from the Amancaya ephitermal Disctrict, Paleocene-Eocene metallogenic belt, II Region, Northern Chile

LÓPEZ, PAOLA; SALVIOLI, MELISA ARIANA; CURCI, MARCELA; PAÉZ, GERARDO; GUIDO, DIEGO

Simposio; 15th Quadrennial Symposium of the International Association on the Genesis of Ore Deposits (IAGOD); 2018

Fluid inclusion (FI) allows to determine the initial condition of the fluid as temperature and salinity. On epithermal systems, this could be a good exploration guide. In this preliminary study we characterize two different stages of the hydrothermal infill of the Central Vein system, the main structure of the Amancaya District, a large epithermal system located in the II Region of Chile.