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Experimental Subsolidus Studies on Epidote Minerals

2004; Mineralogical Society of America; Volume: 56; Issue: 1 Linguagem: Inglês

10.2138/gsrmg.56.1.171

1943-2666

Stefano Poli, Max W. Schmidt,

High-pressure geophysics and materials

Research Article| January 02, 2004 Experimental Subsolidus Studies on Epidote Minerals Stefano Poli; Stefano Poli Dipartimento di Scienze della Terra, Università degli Studi di Milano, Via Botticelli 23, 20133 Milano, Italy Search for other works by this author on: GSW Google Scholar Max W. Schmidt Max W. Schmidt Institute for Mineralogy and Petrology, ETH, 8092 Zürich, Switzerland Search for other works by this author on: GSW Google Scholar Author and Article Information Stefano Poli Dipartimento di Scienze della Terra, Università degli Studi di Milano, Via Botticelli 23, 20133 Milano, Italy Max W. Schmidt Institute for Mineralogy and Petrology, ETH, 8092 Zürich, Switzerland Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2004) 56 (1): 171–195. https://doi.org/10.2138/gsrmg.56.1.171 Article history First Online: 03 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 Stefano Poli, Max W. Schmidt; Experimental Subsolidus Studies on Epidote Minerals. Reviews in Mineralogy and Geochemistry 2004;; 56 (1): 171–195. doi: https://doi.org/10.2138/gsrmg.56.1.171 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 Despite the fact that epidote group minerals are very typical for metamorphism at very low pressure, e.g., in geothermal fields (Bird and Spieler 2004), the first successful synthesis of zoisite and epidotess was reported by Coes (1955) in a paper in the Journal of American Ceramic Society entitled "High pressure minerals." Synthesis conditions were 1 GPa at 800°C; zoisite was obtained from a mixture of kaolin, SiO2, CaO, and CaCl2, whereas epidote was formed by adding FeCl2•H2O to the previous mixture. Once experimental facilities enabled pressures exceeding a few... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.