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Research Article| January 02, 2004 Epidote Group Minerals in Low–Medium Pressure Metamorphic Terranes Rodney H. Grapes; Rodney H. Grapes Institut für Mineralogie, Petrologie und Geochemie, Albert-Ludwigs-Universität Freiburg, Albertstrasse 23 b, D-79104 Freiburg, Germany, rodney.grapes@minpet.uni-freiburg.de, paul.hoskin@minpet.uni-freiburg.de Search for other works by this author on: GSW Google Scholar Paul W. O. Hoskin Paul W. O. Hoskin Institut für Mineralogie, Petrologie und Geochemie, Albert-Ludwigs-Universität Freiburg, Albertstrasse 23 b, D-79104 Freiburg, Germany, rodney.grapes@minpet.uni-freiburg.de, paul.hoskin@minpet.uni-freiburg.de Search for other works by this author on: GSW Google Scholar Author and Article Information Rodney H. Grapes Institut für Mineralogie, Petrologie und Geochemie, Albert-Ludwigs-Universität Freiburg, Albertstrasse 23 b, D-79104 Freiburg, Germany, rodney.grapes@minpet.uni-freiburg.de, paul.hoskin@minpet.uni-freiburg.de Paul W. O. Hoskin Institut für Mineralogie, Petrologie und Geochemie, Albert-Ludwigs-Universität Freiburg, Albertstrasse 23 b, D-79104 Freiburg, Germany, rodney.grapes@minpet.uni-freiburg.de, paul.hoskin@minpet.uni-freiburg.de Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2004) 56 (1): 301–345. https://doi.org/10.2138/gsrmg.56.1.301 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 Rodney H. Grapes, Paul W. O. Hoskin; Epidote Group Minerals in Low–Medium Pressure Metamorphic Terranes. Reviews in Mineralogy and Geochemistry 2004;; 56 (1): 301–345. doi: https://doi.org/10.2138/gsrmg.56.1.301 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 Epidote group minerals are common in metamorphosed mafic to intermediate igneous rocks, quartzofeldspathic sediments and calc-alumina silicate (marl) rocks of higher grade zeolite to medium grade amphibolite facies of low–medium pressure contact and regional metamorphic terranes (i.e., pressure and temperature conditions below the calcite-to-aragonite transition). Within any one rock, epidote composition in terms of Fe3+/(Fe3+ + Al) can be variable, but in general, is limited by whole-rock composition, such that epidote group minerals in metabasite lithologies are more Fe-rich than those in marls that tend to be more Al-rich and typically include zoisite. Because of their wide... 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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