The chromium and nickel distribution in basaltic rocks and eclogites

Details The chromium and nickel distribution in basaltic rocks and eclogites The chromium and nickel distribution in basaltic rocks and eclogites

Jul 1963

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1963gecoa..27..835t&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 27, Issue 7, pp.835-846

Computer Science

4

Scientific paper

Covariance of chromium and nickel in basaltic rocks has been observed for a worldwide sampling and during fractional crystallization of a basaltic magma suggesting preservation of the chromium-nickel ratio from the source of basaltic magma. In eclogites there is a very low nickel content of the garnet phase compared to the pyroxene phase while chromium is more equally distributed between the two phases. This may be of use in evaluating models of the origin of tholeiitic and alkali basalts.

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