The physical and chemical evolution of low-salinity magmatic fluids at the porphyry to epithermal transition: a thermodynamic study
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- 9 February 2005
- journal article
- research article
- Published by Springer Nature in Mineralium Deposita
- Vol. 39 (8) , 864-889
- https://doi.org/10.1007/s00126-004-0461-9
Abstract
No abstract availableKeywords
This publication has 105 references indexed in Scilit:
- Gold solubility, speciation, and partitioning as a function of HCl in the brine-silicate melt-metallic gold system at 800°C and 100 MPaGeochimica et Cosmochimica Acta, 2002
- The Origin of Cu/Au Ratios in Porphyry-Type Ore DepositsScience, 2002
- Gold Solubility in Supercritical Hydrothermal Brines Measured in Synthetic Fluid InclusionsScience, 1999
- Fluid inclusion studies of the Chinkuashih high-sulfidation gold–copper deposits in TaiwanChemical Geology, 1999
- Sulfur evolution of oxidized arc magmas as recorded in apatite from a porphyry copper batholithGeology, 1998
- Characteristics and controls of the largest porphyry copper‐gold and epithermal gold deposits in the circum‐Pacific regionAustralian Journal of Earth Sciences, 1997
- Erosion and collapse of volcanoes: Causes of telescoping in intrusion-centered ore depositsGeology, 1994
- White Island, New Zealand, volcanic-hydrothermal system represents the geochemical environment of high-sulfidation Cu and Au ore depositionGeology, 1993
- Subduction, arc reversal, and the origin of porphyry copper-gold deposits in island arcsGeology, 1990
- High copper content of fluid inclusions in quartz from northern Sonora: Implications for ore-genesis theoryGeology, 1981