Ferric Iron in Feldspar as an Indicator of Evolution of Planetary Oxygen Fugacity

Details Ferric Iron in Feldspar as an Indicator of Evolution of Planetary Oxygen Fugacity Ferric Iron in Feldspar as an Indicator of Evolution of Planetary Oxygen Fugacity

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1065d&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1065

Computer Science

5

Scientific paper

Synchrotron micro-XANES analysis of felsic magma constituents allows us
to constrain independently Fe3+ and hence the oxygen fugacity of
magmatic systems. We focus here on feldspar from anorthosites and
intrusive complexes found on four different bodies.

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