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Normal to inverse transition in Martian spinel; understanding the interplay between chromium, vanadi...

Normal to inverse transition in Martian spinel; understanding the interplay between chromium, vanadi...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_1872593397

Normal to inverse transition in Martian spinel; understanding the interplay between chromium, vanadium, and iron valence state partitioning through a crystal-chemical lens

About this item

Full title

Normal to inverse transition in Martian spinel; understanding the interplay between chromium, vanadium, and iron valence state partitioning through a crystal-chemical lens

Publisher

Washington: Mineralogical Society of America

Journal title

The American mineralogist, 2015-10, Vol.100 (10), p.2018-2025

Language

English

Formats

Publication information

Publisher

Washington: Mineralogical Society of America

More information

Scope and Contents

Contents

Spinel is a very important rock-forming mineral that is found in basalts from Earth, Mars, the Earth's Moon, and basaltic meteorites. Spinel can be used as a sensitive indicator of petrologic and geochemical processes that occur in its host rock. This paper highlights the role of increasing fO2 (from IW-1 to FMQ+2) in converting a >90% normal spine...

Alternative Titles

Full title

Normal to inverse transition in Martian spinel; understanding the interplay between chromium, vanadium, and iron valence state partitioning through a crystal-chemical lens

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_1872593397

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_1872593397

Other Identifiers

ISSN

0003-004X

E-ISSN

1945-3027

DOI

10.2138/am-2015-5208

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