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Experimental hydration of natural volcanic clinopyroxene phenocrysts under hydrothermal pressures (0...

Experimental hydration of natural volcanic clinopyroxene phenocrysts under hydrothermal pressures (0...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_swepub_primary_oai_DiVA_org_uu_304398

Experimental hydration of natural volcanic clinopyroxene phenocrysts under hydrothermal pressures (0.5-3 kbar)

About this item

Full title

Experimental hydration of natural volcanic clinopyroxene phenocrysts under hydrothermal pressures (0.5-3 kbar)

Publisher

Washington: Mineralogical Society of America

Journal title

The American mineralogist, 2016-10, Vol.101 (10), p.2233-2247

Language

English

Formats

Publication information

Publisher

Washington: Mineralogical Society of America

More information

Scope and Contents

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...

Alternative Titles

Full title

Experimental hydration of natural volcanic clinopyroxene phenocrysts under hydrothermal pressures (0.5-3 kbar)

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_swepub_primary_oai_DiVA_org_uu_304398

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_swepub_primary_oai_DiVA_org_uu_304398

Other Identifiers

ISSN

0003-004X,1945-3027

E-ISSN

1945-3027

DOI

10.2138/am-2016-5711CCBYNCND

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