Volatile/mobile trace elements in Karoonda /C4/ chondrite

Details Volatile/mobile trace elements in Karoonda /C4/ chondrite Volatile/mobile trace elements in Karoonda /C4/ chondrite

Sep 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977gecoa..41.1398m&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 41, Sept. 1977, p. 1398-1401.

Computer Science

2

Carbonaceous Chondrites, Meteoritic Composition, Trace Elements, Volatility, Bismuth, Indium, Metamorphism (Geology), Neutron Activation Analysis, Thallium

Scientific paper

Concentrations of ten volatile/mobile trace elements and of nonvolatile Co in the Karoonda (C4) meteorite were determined, and the atomic abundances relative to C1 are compared with values for the Murchison (C2) and Allende (C3) meteorites. Empirical Bi, In, and Tl data for Karoonda and heated Allende and Murchison are compared with theoretical curves for condensation from a gas of cosmic composition at low pressures. It is suggested that Karoonda might derive from low-temperature open-system metamorphism of pristine C3-like material.

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