Polymetallic assemblages with precious metal tellurides and sulfosalts from the Furtei epithermal Au deposit, Sardinia, Italy: Paragenesis and genetic significance

Author:

Fadda S.,Fiori M.,Grillo S. M.,Matzuzzi C.

Publisher

Springer Berlin Heidelberg

Reference12 articles.

1. Afifi AM, Kelly WC, Essene EJ (1988b) Phase relations among tellurides, sulfides, and oxides: II. Applications to telluride bearing ore deposits. Econ Geol 83: 395–404

2. Cook NJ, Ciobanu CL (2002) Tellurides: more than mineralogical curiosities, but also markers of fS2-fO2 evolution in zoned hydrothermal systems. IMA, 18th General Meeting, Edinburg, Programme with Abstracts: 283

3. Cooke DR, McPhail DC (2001) Epithermal Au-Ag-Te mineralization, Acupan, Baguio District, Philippines: numerical simulations of mineral deposition. Econ Geol 96: 109–131

4. Einaudi MT, Hedenquist JW, Inan EE (2003) Sulfidation state of hydrothermal fluids: the porphyry-epithermal transition and beyond. In: Simmons SF, Graham IJ, (eds), Volcanic, geothermal and oreforming fluids: Rulers and whitnesses of processes within the Earth. SEG-Geochem Soc Special Publication 10: 285–313

5. Fiori M, Grillo SM (2001) The Furtei high-sulfidation epithermal gold deposit (Sardinia, Italy): mineral assemblage and its evolution. In: A Piestrzynski et al. (eds), Mineral Deposits at the beginning of the 21st Century, Swets & Zeitlinger: 739–742

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