Abstract
Research Article| January 01, 2011 The Role of Magmatic Sulfur in the Formation of Ore Deposits Adam C. Simon; Adam C. Simon Department of Geoscience and High Pressure Science and Engineering Center (HiPSEC), University of Nevada Las Vegas, Las Vegas, Nevada 89154, U.S.A., adam.simon@unlv.edu Search for other works by this author on: GSW Google Scholar Edward M. Ripley Edward M. Ripley Department of Geological Sciences, Indiana University, Bloomington, Indiana 47405, U.S.A. Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2011) 73 (1): 513–578. https://doi.org/10.2138/rmg.2011.73.16 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Adam C. Simon, Edward M. Ripley; The Role of Magmatic Sulfur in the Formation of Ore Deposits. Reviews in Mineralogy and Geochemistry 2011;; 73 (1): 513–578. doi: https://doi.org/10.2138/rmg.2011.73.16 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 This chapter focuses on S in porphyry-type ore deposits, layered-mafic-intrusion-hosted ore bodies, and magmatic sulfide deposits. Porphyry-type ore deposits, e.g., Bingham Canyon, Utah, U.S.A. and Grasberg, Irian Jaya, are important hosts of Cu, Mo, Au, and Ag. Ore deposits hosted in layered mafic intrusions, e.g., the Bushveld and Stillwater complexes, contain significant quantities of Ni, Cu, Cr, Au and the platinum group elements (PGE: Pt, Pd, Rh, Re, Ir, Ru). Magmatic sulfide deposits, differentiated from layered mafic intrusions in that the former evince more clearly a role for immiscible sulfide accumulation without the possible presence of an aqueous fluid(s), e.g.,... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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