Behavior of Micas at High-Pressure and High-Temperature

Research Article| January 01, 2002 Behavior of Micas at High-Pressure and High-Temperature Pier Francesco Zanazzi; Pier Francesco Zanazzi Dipartimento di Scienze della Terra, Universitá degli Studi di Perugia, Piazza Università, Perugia, Italy, e-mail: zanazzi@unipg.it Search for other works by this author on: GSW Google Scholar Alessandro Pavese Alessandro Pavese Dipartimento di Scienze della Terra, Università degli Studi di Milano, Via Botticelli 23, 20133 Milano, Italy, e-mail: alessandro.pavese@unimi.it Search for other works by this author on: GSW Google Scholar Author and Article Information Pier Francesco Zanazzi Dipartimento di Scienze della Terra, Universitá degli Studi di Perugia, Piazza Università, Perugia, Italy, e-mail: zanazzi@unipg.it Alessandro Pavese Dipartimento di Scienze della Terra, Università degli Studi di Milano, Via Botticelli 23, 20133 Milano, Italy, e-mail: alessandro.pavese@unimi.it Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2002) 46 (1): 99–116. https://doi.org/10.2138/rmg.2002.46.02 Article history First Online: 09 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 Pier Francesco Zanazzi, Alessandro Pavese; Behavior of Micas at High-Pressure and High-Temperature. Reviews in Mineralogy and Geochemistry 2002;; 46 (1): 99–116. doi: https://doi.org/10.2138/rmg.2002.46.02 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 Micas have been long known to play a crucial role in most petrologic and petrogenetic processes, both in magmatic and metamorphic environments. Understanding the crystal-chemical and thermoelastic behavior of this mineral family with variations in pressure (P), temperature (T) and composition (X) is crucial to provide a reliable basis for further interpretation and prediction of phase equilibria, transformations and most reactions occurring in a variety of rocks. In addition, the development of geothermometers and geobarometers has extensively made use of compositional (Fe/Mg+Fe ratio, K/Na+K ratio, Tschermak substitution, etc.) and structural (cation ordering, polytypic occurrence,... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.