Diffusion in Carbonates, Fluorite, Sulfide Minerals, and Diamond

Abstract

Research Article| January 01, 2010 Diffusion in Carbonates, Fluorite, Sulfide Minerals, and Diamond D.J. Cherniak D.J. Cherniak Department of Earth & Environmental Sciences, Rensselaer Polytechnic Institute Troy, New York 12180, U.S.A., chernd@rpi.edu Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2010) 72 (1): 871–897. https://doi.org/10.2138/rmg.2010.72.19 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 D.J. Cherniak; Diffusion in Carbonates, Fluorite, Sulfide Minerals, and Diamond. Reviews in Mineralogy and Geochemistry 2010;; 72 (1): 871–897. doi: https://doi.org/10.2138/rmg.2010.72.19 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 diffusion in non-silicate minerals that do not fall under any of the other chapter categories. This includes minerals that are not oxides (fluorite, sulfide minerals, diamond) and those, like the carbonates, that are not among the oxide minerals discussed in Chapter 17 of this volume (Van Orman and Crispin 2010). Although there are numerous minerals in these categories, limited diffusion data exist for many of them, so the primary phases that will be considered are carbonates, fluorite, diamond, and sulfide minerals. Carbonate minerals are major constituents of sediments and many sedimentary rocks. Fractionation of... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.