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

Fontboté, Lluís; Bendezú, Ronner

Proceedings chapter

English

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

ContributorsFontboté, Lluís; Bendezú, Ronner

Presented atLondon (England), 22-25 August 1999

Published inC.J. Stanley et al. (Ed.), Mineral deposits: processes to processing, Proceedings of the 5th biennial SGA meeting, p. 495-498

PublisherRotterdam

Publication date1999

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.

Affiliation entities

Research groups

Mineral Resources and Geofluids

Citation (ISO format)

FONTBOTÉ, Lluís, BENDEZÚ, Ronner. The carbonate-hosted Zn-Pb San Gregorio deposit (Colquijirca District, Central Peru) as part of a high sulfidation epithermal system. In: Mineral deposits: processes to processing, Proceedings of the 5th biennial SGA meeting. C.J. Stanley et al. (Ed.). London (England). Rotterdam : [s.n.], 1999. p. 495–498.

Proceedings chapter (Accepted version)

Identifiers

PID : unige:29407

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

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