Research Article| January 01, 2008 Deciphering Magma Chamber Dynamics from Styles of Compositional Zoning in Large Silicic Ash Flow Sheets Olivier Bachmann; Olivier Bachmann Department of Earth and Space Sciences, University of Washington, Mailstop 351310, Seattle, Washington, 98195-1310, U.S.A., bachmano@u.washington.edu, bergantz@u.washington.edu Search for other works by this author on: GSW Google Scholar George W. Bergantz George W. Bergantz Department of Earth and Space Sciences, University of Washington, Mailstop 351310, Seattle, Washington, 98195-1310, U.S.A., bachmano@u.washington.edu, bergantz@u.washington.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Olivier Bachmann Department of Earth and Space Sciences, University of Washington, Mailstop 351310, Seattle, Washington, 98195-1310, U.S.A., bachmano@u.washington.edu, bergantz@u.washington.edu George W. Bergantz Department of Earth and Space Sciences, University of Washington, Mailstop 351310, Seattle, Washington, 98195-1310, U.S.A., bachmano@u.washington.edu, bergantz@u.washington.edu Publisher: Mineralogical Society of America First Online: 13 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2008) 69 (1): 651–674. https://doi.org/10.2138/rmg.2008.69.17 Article history First Online: 13 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Olivier Bachmann, George W. Bergantz; Deciphering Magma Chamber Dynamics from Styles of Compositional Zoning in Large Silicic Ash Flow Sheets. Reviews in Mineralogy and Geochemistry 2008;; 69 (1): 651–674. doi: https://doi.org/10.2138/rmg.2008.69.17 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 understanding of the dynamic processes in magmatic systems has grown and changed markedly in the last decade. Old models for magmatic systems as vats of near-liquidus material have been revised by observations from seismology (Sinton and Detrick 1992), crystal chemistry and zoning (Davidson et al. 2007) and the geochronology and geochemistry of both plutonic and volcanic systems (Hildreth 2004; Charlier et al. 2007; Miller et al. 2007; Peressini et al. 2007; Walker et al. 2007). New views emphasise magmatic systems as temporally dominated by crystal mushes (magma bodies with... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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