RESEARCH GROUP

button mineral resources
Mineral Resources and Geofluids
 

Ore Deposits Introductory Course

Prof. Lluís Fontboté and collaborators

 

Slides to Chapter B4

Hydrothermal Alteration

Examples of high sulfidation zonation

Refugio

Typical zonation formed by very acid high sulfidation fluids.
From center to flanks: Residual silica (dark brown), kaolinite-alunite (white), kaolinite-sericite light brown.
Refugio Mine, Maricunga Belt, northern Chile.
Photo Lluís Fontboté, 1994.10-4/06 Copyright © 1999 - Lluís Fontboté - All Rights Reserved.

 

Examples of residual silica/vuggy silica

Colquijirca

Typical vuggy (or residual) silica in the central part of the Marcapunta Au-Ag prospect,
Colquijirca District, Central Peru
Photo Lluís Fontboté, 1998.3/11 Copyright © 1999 - Lluís Fontboté - All Rights Reserved.

 

Colquijirca

Alunite-filled former K-Fd phenocryst in vuggy silica, Marcapunta Au-Ag prospect,
Colquijirca District, Central Peru.
(Photo Lluís Fontboté, 11998.3/06) Copyright © 1999 - Lluís Fontboté - All Rights Reserved.

See also other examples of high sulfidation systems

 

[Mineral Resources and Geofluids]

 


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