Fluid evolution in the W-Cu-Zn-Pb San Cristobal vein, Peru: fluid inclusion and stable isotope evidence

Beuchat, Sebastien; Moritz, Robert; Pettke, T.

doi:10.1016/j.chemgeo.2004.06.008

Scientific article

English

Fluid evolution in the W-Cu-Zn-Pb San Cristobal vein, Peru: fluid inclusion and stable isotope evidence

ContributorsBeuchat, Sebastien; Moritz, Robert; Pettke, T.

Published inChemical geology, vol. 210, no. 1-4, p. 201-224

Publication date2004

Keywords

Fluid inclusion
Stable isotope
Laser ablation
Ore deposit
Hydrothermal fluid

Affiliation entities

Faculté des sciences / Section des sciences de la Terre et de l'Environnement / Département de minéralogie
Faculté des sciences / Section des sciences de la Terre et de l'Environnement / Département des sciences de la Terre

Research groups

Mineral Resources and Geofluids

Citation (ISO format)

BEUCHAT, Sebastien, MORITZ, Robert, PETTKE, T. Fluid evolution in the W-Cu-Zn-Pb San Cristobal vein, Peru: fluid inclusion and stable isotope evidence. In: Chemical geology, 2004, vol. 210, n° 1-4, p. 201–224. doi: 10.1016/j.chemgeo.2004.06.008

Article (Published version)

Identifiers

PID : unige:21625
DOI : 10.1016/j.chemgeo.2004.06.008

Additional URL for this publicationhttp://linkinghub.elsevier.com/retrieve/pii/S0009254104001998

Journal ISSN0009-2541

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Fluid evolution in the W-Cu-Zn-Pb San Cristobal vein, Peru: fluid inclusion and stable isotope evidence

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