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 Petrogenesis and Parent Body
About this item
Full title
Author / Creator
Publisher
Hampton: NASA/Langley Research Center
Journal title
Language
English
Formats
Publication information
Publisher
Hampton: NASA/Langley Research Center
Subjects
More information
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
Authors, Artists and Contributors
Author / Creator
Identifiers
Primary Identifiers
Record Identifier
TN_cdi_proquest_journals_2128105640
Permalink
https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2128105640