Defining the Terrestrial Oxygen Isotope Fractionation Line and Observed Oxygen Isotopic Heterogeneity Within the Allende Meteorite

Details Defining the Terrestrial Oxygen Isotope Fractionation Line and Observed Oxygen Isotopic Heterogeneity Within the Allende Meteorite Defining the Terrestrial Oxygen Isotope Fractionation Line and Observed Oxygen Isotopic Heterogeneity Within the Allende Meteorite

Mar 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011lpi....42.1827p&link_type=abstract

42nd Lunar and Planetary Science Conference, held March 7–11, 2011 at The Woodlands, Texas. LPI Contribution No. 1608, p.1827

Computer Science

Scientific paper

We show that the O isotope terrestrial fractionation line does not pass
through the origin. Allende is isotopically heterogeneous (on 0.3 g
scale) with no correlation with the chemical composition.

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