Isotopic variations of germanium in iron and stony iron meteorites

Details Isotopic variations of germanium in iron and stony iron meteorites Isotopic variations of germanium in iron and stony iron meteorites

Oct 1997

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1997gecoa..61.4439h&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 61, p. 4439

Computer Science

6

Stony-Iron Meteorites, Germanium Isotopes, Iron Meteorites, Meteoritic Composition, Mass Spectrometers, Plasma Spectra, Fractionation

Scientific paper

A multiple collector-inductively coupled plasma mass spectrometer, together with Ga external correction techniques, are presently used to determine the Ge isotopic ratios for several iron meteorites as well as germanite and three Ge shelf standards. The Ge isotopic compositions for IAB nonmagmatic irons show wide variations covering almost the entire range of iron meteorites in this study. The Ge in IAB nonmagmatic irons are therefore implied to have been fractionated by the Ge partial evaporation process.

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