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Fluid Immiscibility in Volcanic Environments

2007; Mineralogical Society of America; Volume: 65; Issue: 1 Linguagem: Inglês

10.2138/rmg.2007.65.10

1943-2666

James D. Webster, Charles W. Mandeville,

earthquake and tectonic studies

Research Article| July 01, 2007 Fluid Immiscibility in Volcanic Environments James D. Webster; James D. Webster Department of Earth and Planetary Sciences, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024-5192 U.S.A., jdw@amnh.org, cmandy@amnh.org Search for other works by this author on: GSW Google Scholar Charles W. Mandeville Charles W. Mandeville Department of Earth and Planetary Sciences, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024-5192 U.S.A., jdw@amnh.org, cmandy@amnh.org Search for other works by this author on: GSW Google Scholar Author and Article Information James D. Webster Department of Earth and Planetary Sciences, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024-5192 U.S.A., jdw@amnh.org, cmandy@amnh.org Charles W. Mandeville Department of Earth and Planetary Sciences, American Museum of Natural History, Central Park West at 79th Street, New York, New York 10024-5192 U.S.A., jdw@amnh.org, cmandy@amnh.org Publisher: Mineralogical Society of America First Online: 09 Mar 2017 © The Mineralogical Society Of America Reviews in Mineralogy and Geochemistry (2007) 65 (1): 313–362. https://doi.org/10.2138/rmg.2007.65.10 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 James D. Webster, Charles W. Mandeville; Fluid Immiscibility in Volcanic Environments. Reviews in Mineralogy and Geochemistry 2007;; 65 (1): 313–362. doi: https://doi.org/10.2138/rmg.2007.65.10 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 Volatile components enter the atmosphere, oceans, and other surface waters through pre-, syn-, and post-eruptive volcanic processes that involve a variety of fluids. Aluminosilicate-poor fluids include aqueous or carbonic to sulfide-, sulfate-, chloride-, fluoride-, carbonate-, and phosphate-rich compositions in volcanic environments, but other more complex combinations of these constituents may be involved (Giggenbach 1977; Roedder 1984, 1992; Lowenstern 1995). Other, rare gases and dissolved constituents (e.g., H2, N2, He, Ar, H3BO3, Hg, CH4 and other hydrocarbon compounds, metals, and metalloids) are also present, but in general... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.