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Aster Deep Learning alteration mineral mapping of the Cerro Casale & Caspiche porphyry gold-copper deposits

Cerro Casale and Caspiche Porphyr Gold-Copper Deposits

The gold and copper in the Cerro Casale deposit is most directly associated with quartz-sulfide-magnetite stock work veins and veinlets in potassic altered rocks.

High-sulphidation epithermal, intermediate sulphidation epithermal and porphyry-style mineralization occur at the Caspiche deposit. 

High-sulphidation epithermal-style alteration outcrops at Caspiche Porphyry, and hosts disseminated gold in felsic volcanic rocks and dioritic to quartz dioritic quartz-feldspar porphyry intrusive rocks.

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The Cerro Casale and the Caspiche Au Cu deposits were discovered in the 1980s

Location of the Cerro Casale and Caspiche porphyry Au Cu
deposits.
Colour image of a 14 band ASTER satellite photo taken on February
9, 2005.

Detection of important alteration minerals.

We have conducted Deep Learning alteration mineral mapping tests and verification on epithermal, porphyry and carbonate replacement deposits.

Colour image of a 14 band ASTER satellite photo.

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