Thermochemistry of Sulfide Mineral Solutions

Research Article| January 01, 2006 Thermochemistry of Sulfide Mineral Solutions Richard O. Sack; Richard O. Sack OFM Research, 28430 NE 47th Place, Redmond, Washington, 98053-8841, U.S.A., e-mail: fahlore@centurytel.net or rosack@ofm-research.org Search for other works by this author on: GSW Google Scholar Denton S. Ebel Denton S. Ebel Department of Earth and Planetary Sciences, American Museum of Natural History, Central Park West at 79th Street, New York, New York, 10024-5192, U.S.A., e-mail: debel@amnh.org or dsebel@ofm-research.org Search for other works by this author on: GSW Google Scholar Author and Article Information Richard O. Sack OFM Research, 28430 NE 47th Place, Redmond, Washington, 98053-8841, U.S.A., e-mail: fahlore@centurytel.net or rosack@ofm-research.org Denton S. Ebel Department of Earth and Planetary Sciences, American Museum of Natural History, Central Park West at 79th Street, New York, New York, 10024-5192, U.S.A., e-mail: debel@amnh.org or dsebel@ofm-research.org Publisher: Mineralogical Society of America First Online: 13 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2006) 61 (1): 265–364. https://doi.org/10.2138/rmg.2006.61.6 Article history First Online: 13 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Richard O. Sack, Denton S. Ebel; Thermochemistry of Sulfide Mineral Solutions. Reviews in Mineralogy and Geochemistry 2006;; 61 (1): 265–364. doi: https://doi.org/10.2138/rmg.2006.61.6 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 SocietyReviews in Mineralogy and Geochemistry Search Advanced Search In the sulfide mineral assemblages commonly found in terrestrial rocks, the major elements are S with the metals Fe, Zn, Cu, Pb, and Ag and semimetals As and Sb. Minor elements include Te, Se; the metals Ni, Cd, Co, Mn and the semimetals Hg and Bi. Particular ore deposits can be characterized using specific subsystems containing these elements (e.g., McKinstry 1963). Previous reviews have summarized in detail the phase relations in binary, ternary, and higher-order systems. These include Barton (1970), the first volume in this series (Craig and Scott 1976), excellent chapters by Barton and Skinner... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.