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Palai-Islica Au-Cu Deposit Analysis by Stone is a document available to read on EtoBox.
This document summarizes two types of epithermal mineralization identified in the Palai-Islica Au-Cu deposit in Spain: 1) Intermediate sulfidation hosted by quartz veins with pyrite, chalcopyrite, sphalerite and galena as major sulfides. Fluid inclusions indicate temperatures of 118-453°C and salinities of 0.2-51.4% NaCl. 2) High sulfidation consisting of massive silicification with disseminated pyrite and minor copper minerals. Fluid inclusions indicate temperatures of 224-381°C and salinities of 0.4-41.1%
- Author
- Stone
- Language
- EN