Nickel isotopic studies in meteorites

Details Nickel isotopic studies in meteorites Nickel isotopic studies in meteorites

May 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983e%26psl..63..167m&link_type=abstract

Earth and Planetary Science Letters (ISSN 0012-821X), vol. 63, no. 2, May 1983, p. 167-176.

Computer Science

14

Abundance, Cosmochemistry, Meteoritic Composition, Nickel Isotopes, Carbonaceous Chondrites, Chemical Composition, Iron Meteorites, Mass Spectroscopy, Nuclear Fusion, Meteorites, Isotopes, Composition, Nickel, Analysis, Mass Spectrometry, Samples, Meteorite, Anomalies, Catalog, C1 Chondrites, C3 Chondrites, L Chondrites, Ll Chondrites, H Chondrites, E Chondrites, Allende, Ivb Iron Meteorites, Eagle Station, Pallasites, Inclusions, Matrix

Scientific paper

The nickel isotopic composition of meteoritic materials is analyzed by high-precision mass spectrometry. The samples treated include almost all the meteorite types for which large isotopic anomalies have been reported for oxygen, silver, magnesium, and titanium. The samples are Cl, C3, L, LL, H and E chondrites, IVB irons, Eagle Station pallasite, and inclusion, matrix and 'whole rock' samples of the Allende meteorite. No anomaly is found for nickel isotopic compositions within an accuracy of 0.7 part per thousand for Ni-61/Ni-60, 0.4-0.08 part per thousand for Ni-62/Ni-60, and 1-1.5 parts per thousand for Ni-64/Ni-60.

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