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• W2009958649 abstract "Research Article| September 01, 2004 Magmatic vapor contraction and the transport of gold from the porphyry environment to epithermal ore deposits Christoph A. Heinrich; Christoph A. Heinrich 1Department of Earth Sciences, Swiss Federal Institute of Technology, ETH Zentrum NO, 8092 Zürich, Switzerland Search for other works by this author on: GSW Google Scholar Thomas Driesner; Thomas Driesner 1Department of Earth Sciences, Swiss Federal Institute of Technology, ETH Zentrum NO, 8092 Zürich, Switzerland Search for other works by this author on: GSW Google Scholar Andri Stefánsson; Andri Stefánsson 1Department of Earth Sciences, Swiss Federal Institute of Technology, ETH Zentrum NO, 8092 Zürich, Switzerland Search for other works by this author on: GSW Google Scholar Terry M. Seward Terry M. Seward 1Department of Earth Sciences, Swiss Federal Institute of Technology, ETH Zentrum NO, 8092 Zürich, Switzerland Search for other works by this author on: GSW Google Scholar Author and Article Information Christoph A. Heinrich 1Department of Earth Sciences, Swiss Federal Institute of Technology, ETH Zentrum NO, 8092 Zürich, Switzerland Thomas Driesner 1Department of Earth Sciences, Swiss Federal Institute of Technology, ETH Zentrum NO, 8092 Zürich, Switzerland Andri Stefánsson 1Department of Earth Sciences, Swiss Federal Institute of Technology, ETH Zentrum NO, 8092 Zürich, Switzerland Terry M. Seward 1Department of Earth Sciences, Swiss Federal Institute of Technology, ETH Zentrum NO, 8092 Zürich, Switzerland Publisher: Geological Society of America Received: 19 Mar 2004 Revision Received: 20 May 2004 Accepted: 20 May 2004 First Online: 03 Mar 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (2004) 32 (9): 761–764. https://doi.org/10.1130/G20629.1 Article history Received: 19 Mar 2004 Revision Received: 20 May 2004 Accepted: 20 May 2004 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Christoph A. Heinrich, Thomas Driesner, Andri Stefánsson, Terry M. Seward; Magmatic vapor contraction and the transport of gold from the porphyry environment to epithermal ore deposits. Geology 2004;; 32 (9): 761–764. doi: https://doi.org/10.1130/G20629.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Fluid-phase stability relations combined with thermodynamic modeling using fluid-inclusion analyses and new gold-solubility experiments lead to an integrated geological interpretation linking epithermal gold mineralization and porphyry-style ore formation to the cooling of hydrous magma chambers. The essential chemical requirement for gold transport to low temperatures is an initial excess of sulfide over Fe in the magmatic fluid, which is best achieved by condensing out Fe-rich brine from a buoyant, low- to medium-salinity vapor enriched in volatile S. This vapor can contract directly to an aqueous liquid, by cooling at elevated pressure above the critical curve of the salt-water fluid system. Physical and chemical conditions are matched when magmatic fluid is released through a gradually downward-retracting interface of crystallizing magma beneath a porphyry stock, predicting the consistent zoning and overprinting relations of alteration and mineralization observed in magmatic hydrothermal systems. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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