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Title

The carbonate-hosted Zn-Pb San Gregorio deposit (Colquijirca District, Central Peru) as part of a high sulfidation epithermal system

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Published in C.J. Stanley et al. Mineral deposits: processes to processing, Proceedings of the 5th biennial SGA meeting. London (England) - 22-25 August 1999 - Rotterdam. 1999, p. 495-498
Abstract The recently discovered world class San Gregorio Zn-Pb deposit in Central Peru, has formed by high level carbonate replacement through very acid fluids coming from a high sulfidation system related to a Tertiary volcanic neck, which produces also Au-Ag, Cu-Au and Zn-Pb-Ag ores in other parts of the same district. To our knowledge San Gregorio is the first "carbonate-hosted epithermal Zn-Pb high sulfidation deposit" recognized as such.
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Structures
Research group Mineral Resources and Geofluids
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FONTBOTÉ, Lluis, BENDEZÚ, Ronner. The carbonate-hosted Zn-Pb San Gregorio deposit (Colquijirca District, Central Peru) as part of a high sulfidation epithermal system. In: C.J. Stanley et al. (Ed.). Mineral deposits: processes to processing, Proceedings of the 5th biennial SGA meeting. London (England). Rotterdam : [s.n.], 1999. p. 495-498. https://archive-ouverte.unige.ch/unige:29407

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Deposited on : 2013-08-21

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