Epidote in Geothermal Systems

Abstract

Research Article| January 02, 2004 Epidote in Geothermal Systems Dennis K. Bird; Dennis K. Bird Department of Geological and Environmental Sciences Stanford University Stanford, California 94305, U.S.A. Search for other works by this author on: GSW Google Scholar Abigail R. Spieler Abigail R. Spieler Department of Geological and Environmental Sciences Stanford University Stanford, California 94305, U.S.A. Search for other works by this author on: GSW Google Scholar Reviews in Mineralogy and Geochemistry (2004) 56 (1): 235–300. https://doi.org/10.2138/gsrmg.56.1.235 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 Dennis K. Bird, Abigail R. Spieler; Epidote in Geothermal Systems. Reviews in Mineralogy and Geochemistry 2004;; 56 (1): 235–300. doi: https://doi.org/10.2138/gsrmg.56.1.235 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 Early in the 20th Century epidote was readily recognized as a common rock-forming mineral of metamorphic and hydrothermal processes (Becke 1903; Grubenmann 1904; Van Hise 1904; Goldschmidt 1911; Eskola 1915). Its distribution is widespread in the Earth’s crust, including metamorphic environments of pumpellyite-prehnite, greenschist, epidote-amphibolite, and blueschist facies (Seki 1972; Liou 1993). In lower-pressure hydrothermal environments epidote is a common mineral in skarns, in propylitic altered volcanic rocks and in late-stage veins related to silicic intrusions (Lindgren 1933; Coats 1940; Nakovnik 1963). Within obducted segments of oceanic... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.