The Stability of Hydrous Mantle Phases

Research Article| January 01, 2006 The Stability of Hydrous Mantle Phases Daniel J. Frost Daniel J. Frost Bayerisches Geoinstitut, University of Bayreuth, D-95440 Bayreuth, Germany, e-mail: Dan.Frost@uni-bayreuth.de Search for other works by this author on: GSW Google Scholar Author and Article Information Daniel J. Frost Bayerisches Geoinstitut, University of Bayreuth, D-95440 Bayreuth, Germany, e-mail: Dan.Frost@uni-bayreuth.de Publisher: Mineralogical Society of America First Online: 03 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2006) 62 (1): 243–271. https://doi.org/10.2138/rmg.2006.62.11 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 Daniel J. Frost; The Stability of Hydrous Mantle Phases. Reviews in Mineralogy and Geochemistry 2006;; 62 (1): 243–271. doi: https://doi.org/10.2138/rmg.2006.62.11 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 It is widely recognized that hydrous minerals are involved in a number of geochemical processes in the Earth’s mantle (Michael 1988; Thompson 1992; Schmidt and Poli 1998). Their presence affects the onset of melting (Lambert and Wyllie 1968; Mysen and Boettcher 1975) and can control the partitioning of trace elements during partial melting (Adam et al. 1993; Ionov and Hoffmann 1995; La Tourrette et al. 1995; Tiepolo et al. 2000). They have accordingly been implicated in the source regions of many types of magmas including alkaline basalts and highly-potassic... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.