Slides to Chapter B4
Hydrothermal Alteration
Examples of high sulfidation zonation
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 LluÃs Fontboté, 1994.10-4/06 Copyright © 1999 - LluÃs Fontboté - All Rights Reserved.
Examples of residual silica/vuggy silica
Typical vuggy (or residual) silica in the central part of the Marcapunta Au-Ag prospect,
Colquijirca District, Central Peru
Photo LluÃs Fontboté, 1998.3/11 Copyright © 1999 - LluÃs Fontboté - All Rights Reserved.
Alunite-filled former K-Fd phenocryst in vuggy silica, Marcapunta Au-Ag prospect,
Colquijirca District, Central Peru.
(Photo LluÃs Fontboté, 11998.3/06) Copyright © 1999 - LluÃs Fontboté - All Rights Reserved.See also other examples of high sulfidation systems