Alunite-Jarosite Crystallography, Thermodynamics, and Geochronology

Abstract

Research Article| January 01, 2000 Alunite-Jarosite Crystallography, Thermodynamics, and Geochronology R. E. Stoffregen; R. E. Stoffregen AWK Consulting Engineers, Inc., 1611 Monroeville Avenue, Turtle Creek, Pennsylvania 15145 Search for other works by this author on: GSW Google Scholar C. N. Alpers; C. N. Alpers U.S. Geological Survey, Water Resources Division, 6000 J Street Sacramento, California 95819 Search for other works by this author on: GSW Google Scholar J. L. Jambor J. L. Jambor Leslie Research and Consulting, 316 Rosehill Wynd Tsawwassen, British Columbia, Canada V4M 3L9 Search for other works by this author on: GSW Google Scholar Author and Article Information R. E. Stoffregen AWK Consulting Engineers, Inc., 1611 Monroeville Avenue, Turtle Creek, Pennsylvania 15145 C. N. Alpers U.S. Geological Survey, Water Resources Division, 6000 J Street Sacramento, California 95819 J. L. Jambor Leslie Research and Consulting, 316 Rosehill Wynd Tsawwassen, British Columbia, Canada V4M 3L9 Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2000) 40 (1): 453–479. https://doi.org/10.2138/rmg.2000.40.9 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation R. E. Stoffregen, C. N. Alpers, J. L. Jambor; Alunite-Jarosite Crystallography, Thermodynamics, and Geochronology. Reviews in Mineralogy and Geochemistry 2000;; 40 (1): 453–479. doi: https://doi.org/10.2138/rmg.2000.40.9 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 The alunite supergroup consists of more than 40 mineral species that have in common the general formula DG3(TO4)2(OH,H2O)6. The D sites are occupied by monovalent (e.g. K, Na, NH4, Ag, Tl, H3O), divalent (e.g. Ca, Sr, Ba, Pb), trivalent (e.g. Bi, REE) or more rarely quadrivalent (Th) ions; G is Al or Fe3+ or rarely Ga or V; T is S6+, As5+, or P5+, and may include subordinate amounts of Cr6+ or Si4+. Many... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.