Mica Crystal Chemistry and the Influence of Pressure, Temperature, and Solid Solution on Atomistic Models

Research Article| January 01, 2002 Mica Crystal Chemistry and the Influence of Pressure, Temperature, and Solid Solution on Atomistic Models Maria Franca Brigatti; Maria Franca Brigatti Dipartimento di Scienze della Terra, Università di Modena e Reggio Emilia, Via S. Eufemia, 19, I-41100 Modena, Italy, brigatti@unimo.it Search for other works by this author on: GSW Google Scholar Stephen Guggenheim Stephen Guggenheim Department of Earth and Environmental Sciences, University of Illinois at Chicago, 845 West Taylor Street, M/C 186, Chicago, Illinois 60607, xtal@uic.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Maria Franca Brigatti Dipartimento di Scienze della Terra, Università di Modena e Reggio Emilia, Via S. Eufemia, 19, I-41100 Modena, Italy, brigatti@unimo.it Stephen Guggenheim Department of Earth and Environmental Sciences, University of Illinois at Chicago, 845 West Taylor Street, M/C 186, Chicago, Illinois 60607, xtal@uic.edu Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2002) 46 (1): 1–97. https://doi.org/10.2138/rmg.2002.46.01 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 Maria Franca Brigatti, Stephen Guggenheim; Mica Crystal Chemistry and the Influence of Pressure, Temperature, and Solid Solution on Atomistic Models. Reviews in Mineralogy and Geochemistry 2002;; 46 (1): 1–97. doi: https://doi.org/10.2138/rmg.2002.46.01 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 The 2:1 mica layer is composed of two opposing tetrahedral (T) sheets with an octahedral (M) sheet between to form a “TMT” layer (Fig. 1a1). The mica structure has a general formula of A M2–3 T4 O10 X2 [in natural micas: A = interlayer cations, usually K, Na, Ca, Ba, and rarely Rb, Cs, NH4, H3O, and Sr; M = octahedral cations, generally Mg, Fe2+, Al, and Fe3+, but other cations such as Li, Ti, V, Cr, Mn, Co, Ni, Cu, and Zn can occur also... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.