Meteoritic component and impact melt composition at the Lac a l'Eau Claire /Clearwater/ impact structures, Quebec

Details Meteoritic component and impact melt composition at the Lac a l'Eau Claire /Clearwater/ impact structures, Quebec Meteoritic component and impact melt composition at the Lac a l'Eau Claire /Clearwater/ impact structures, Quebec

Apr 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978gecoa..42..429g&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 42, Apr. 1978, p. 429-431.

Computer Science

8

Computer Programs, Geochemistry, Lithology, Meteoritic Composition, Trace Elements, Canada, Chondrites, Cobalt, Melting, Meteorite Craters, Nickel, Orgueil Meteorite, Quartz

Scientific paper

The major and selected trace element composition of the melt at the eastern Lac a l'Eau Claire impact structure can be modelled by 52.3 percent granodiorite, 15.1 percent granulite, 25.7 percent quartz-monzonite plus 6.9 percent Orgueil (Cl-chondrite). A satisfactory fit to melt at the western structure requires 57.4 percent granulite and 42.6 percent quartz-monzonite. These models agree with the suggestions of Palme et al. (1978) on the type and extent of meteoritic component in the melts.

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