Changes in the cell parameters of antigorite close to its dehydration reaction at subduction zone co...
Changes in the cell parameters of antigorite close to its dehydration reaction at subduction zone conditions
About this item
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Author / Creator
Publisher
Washington: Mineralogical Society of America
Journal title
Language
English
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Publisher
Washington: Mineralogical Society of America
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More information
Scope and Contents
Contents
The unit-cell parameter a of antigorite (usually expressed as the polysome m value) has been determined as a function of temperature (T) and pressure (P) in the range of 600-650°C, 25-45 kbar in weeklong piston-cylinder experiments. A well-characterized natural antigorite (with m=16 and less abundant m=15) was used as a starting material that coexi...
Alternative Titles
Full title
Changes in the cell parameters of antigorite close to its dehydration reaction at subduction zone conditions
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Primary Identifiers
Record Identifier
TN_cdi_hal_primary_oai_HAL_hal_02562294v1
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_hal_primary_oai_HAL_hal_02562294v1
Other Identifiers
ISSN
0003-004X
E-ISSN
1945-3027
DOI
10.2138/am-2020-7159
