Melt Inclusions in Basaltic and Related Volcanic Rocks 论文

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Research Article| January 01, 2008 Melt Inclusions in Basaltic and Related Volcanic Rocks Adam J.R. Kent Adam J.R. Kent Department of Geosciences, Oregon State University, Corvallis, Oregon, 97331, U.S.A., adam.kent@geo.oregonstate.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Adam J.R. Kent Department of Geosciences, Oregon State University, Corvallis, Oregon, 97331, U.S.A., adam.kent@geo.oregonstate.edu Publisher: Mineralogical Society of America First Online: 13 Jul 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2008) 69 (1): 273–331. https://doi.org/10.2138/rmg.2008.69.8 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 Adam J.R. Kent; Melt Inclusions in Basaltic and Related Volcanic Rocks. Reviews in Mineralogy and Geochemistry 2008;; 69 (1): 273–331. doi: https://doi.org/10.2138/rmg.2008.69.8 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 Melt inclusions are small parcels of melt trapped in crystals within magmatic systems, and are analogous to fluid inclusions formed by trapping of hydrothermal and other fluids during mineral growth in fluid-mineral systems (Sorby 1858; Roedder 1979, 1984). After trapping, melt inclusions are potentially isolated from external melt and thus provide a way to investigate melts trapped during magmatic evolution—driven by processes such as crystal-liquid separation, vapor saturation and degassing, magma mixing and assimilation—which can dramatically alter the compositions of the eventual erupted (or intruded) magmatic end products. Melt inclusions are a powerful tool for the... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.