Experimental hydration of natural volcanic clinopyroxene phenocrysts under hydrothermal pressures (0...
Experimental hydration of natural volcanic clinopyroxene phenocrysts under hydrothermal pressures (0.5-3 kbar)
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Publisher
Washington: Mineralogical Society of America
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Language
English
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Washington: Mineralogical Society of America
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Contents
Water is a key parameter in mantle rheology, magma genesis, magma evolution, and resulting eruption styles, because it controls the density and the viscosity, as well as the melting and crystallization behavior of a melt. The water content in nominally anhydrous minerals (NAMs) such as clinopyroxene recently has been used as a proxy for magmatic wa...
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Full title
Experimental hydration of natural volcanic clinopyroxene phenocrysts under hydrothermal pressures (0.5-3 kbar)
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TN_cdi_swepub_primary_oai_DiVA_org_uu_304398
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_swepub_primary_oai_DiVA_org_uu_304398
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ISSN
0003-004X,1945-3027
E-ISSN
1945-3027
DOI
10.2138/am-2016-5711CCBYNCND