Magmatic Inclusions in Olivine and Chromite in Basaltic Shergottite Sayh Al Uhaymir 005: Implications for Petrogenesis and Relationship to Lherzolitic Shergottites

Details Magmatic Inclusions in Olivine and Chromite in Basaltic Shergottite Sayh Al Uhaymir 005: Implications for Petrogenesis and Relationship to Lherzolitic Shergottites Magmatic Inclusions in Olivine and Chromite in Basaltic Shergottite Sayh Al Uhaymir 005: Implications for Petrogenesis and Relationship to Lherzolitic Shergottites

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1174g&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1174

Computer Science

4

Scientific paper

SaU 005 has an excess mafic component which may be cumulus, xenolithic,
or an admixed (primitive) magma. Melt inclusions in olivine and chromite
are consistent with any of these, and suggest a link to lherzolitic
shergottites rather than EET 79001A.

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