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The Cr Redox Record of fO2 Variation in Angrites. Evidence for Redox Conditions of Angrite Petrogene...

The Cr Redox Record of fO2 Variation in Angrites. Evidence for Redox Conditions of Angrite Petrogene...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2128105640

The Cr Redox Record of fO2 Variation in Angrites. Evidence for Redox Conditions of Angrite Petrogenesis and Parent Body

About this item

Full title

The Cr Redox Record of fO2 Variation in Angrites. Evidence for Redox Conditions of Angrite Petrogenesis and Parent Body

Publisher

Hampton: NASA/Langley Research Center

Journal title

NASA Center for AeroSpace Information (CASI). Conference Proceedings, 2016

Language

English

Publication information

Publisher

Hampton: NASA/Langley Research Center

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Scope and Contents

Contents

Angrites represent some of the earliest stages of planetesimal differentiation. Not surprisingly, there is no simple petrogenetic model for their origin. Petrogenesis has been linked to both magmatic and impact processes. Studies demonstrated that melting of chondritic material (e.g. CM, CV) at redox conditions where pure iron metal is unstable (e....

Alternative Titles

Full title

The Cr Redox Record of fO2 Variation in Angrites. Evidence for Redox Conditions of Angrite Petrogenesis and Parent Body

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Primary Identifiers

Record Identifier

TN_cdi_proquest_journals_2128105640

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2128105640

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