16O-poor Refractory Inclusions in CB Chondrites

Details 16O-poor Refractory Inclusions in CB Chondrites 16O-poor Refractory Inclusions in CB Chondrites

Mar 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001lpi....32.1229k&link_type=abstract

32nd Annual Lunar and Planetary Science Conference, March 12-16, 2001, Houston, Texas, abstract no.1229

Computer Science

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Scientific paper

CAIs from Hammadah al Hamra 237 and QUE 94411 have 16O-poor compositions
with D17O ranging from -6‰ to -10‰ for all analyzed
minerals (grossite, hibonite, melilite, pyroxene, spinel), suggesting
formation in an isotopically distinct reservoir.

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