Trace-Element Partitioning Between Amphibole and Silicate Melt

Abstract

Research Article| October 01, 2007 Trace-Element Partitioning Between Amphibole and Silicate Melt Massimo Tiepolo; Massimo Tiepolo Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche I-27100 Pavia, Italy, [e-mail], [e-mail], [e-mail] Search for other works by this author on: GSW Google Scholar Roberta Oberti; Roberta Oberti Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche I-27100 Pavia, Italy, [e-mail], [e-mail], [e-mail] Search for other works by this author on: GSW Google Scholar Alberto Zanetti; Alberto Zanetti Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche I-27100 Pavia, Italy, [e-mail], [e-mail], [e-mail] Search for other works by this author on: GSW Google Scholar Riccardo Vannucci; Riccardo Vannucci Dipartimento di Scienze della Terra, Università di Pavia, and Istituto di Geoscienze e Georisorse Consiglio Nazionale delle Ricerche, Pavia, Italy, [e-mail] Search for other works by this author on: GSW Google Scholar Stephen F. Foley Stephen F. Foley Institut für Geowissenschaften Universität Mainz, Mainz, Germany, [e-mail] Search for other works by this author on: GSW Google Scholar Author and Article Information Massimo Tiepolo Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche I-27100 Pavia, Italy, [e-mail], [e-mail], [e-mail] Roberta Oberti Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche I-27100 Pavia, Italy, [e-mail], [e-mail], [e-mail] Alberto Zanetti Istituto di Geoscienze e Georisorse, Consiglio Nazionale delle Ricerche I-27100 Pavia, Italy, [e-mail], [e-mail], [e-mail] Riccardo Vannucci Dipartimento di Scienze della Terra, Università di Pavia, and Istituto di Geoscienze e Georisorse Consiglio Nazionale delle Ricerche, Pavia, Italy, [e-mail] Stephen F. Foley Institut für Geowissenschaften Universität Mainz, Mainz, Germany, [e-mail] Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2007) 67 (1): 417–452. https://doi.org/10.2138/rmg.2007.67.11 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 Massimo Tiepolo, Roberta Oberti, Alberto Zanetti, Riccardo Vannucci, Stephen F. Foley; Trace-Element Partitioning Between Amphibole and Silicate Melt. Reviews in Mineralogy and Geochemistry 2007;; 67 (1): 417–452. doi: https://doi.org/10.2138/rmg.2007.67.11 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 Knowledge of the partitioning behavior of trace elements between solid and liquid is a prerequisite for modern igneous and mantle petrology. Most of the mathematical models simulating melt generation, migration and evolution within the mantle and/or the crust require the availability of reliable solid/liquid partition coefficients for the mineral phases involved in the process. Calcic amphiboles are extremely important for the understanding of lithospheric processes because of both their common occurrence in a variety of igneous and metamorphic rocks types and their capability of hosting a large number of geochemically important trace elements. A series of studies on the partitioning... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.