Fractionation of fluorine, chlorine and other trace elements during differentiation of a tholeiitic magma

Details Fractionation of fluorine, chlorine and other trace elements during differentiation of a tholeiitic magma Fractionation of fluorine, chlorine and other trace elements during differentiation of a tholeiitic magma

Sep 1966

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1966gecoa..30..963g&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 30, Issue 9, pp.963-982

Physics

6

Scientific paper

The elements F, Cl, Ni, Co, Cu, Ga, Sc, Cr, V, Ba and Sr have been determined in two drill cores through a differentiated tholeiitic dolerite sill from Tasmania. A multivariate statistical technique is employed to demonstrate the occupancy of hydroxyl lattice sites by both chlorine and fluorine. Consideration of trace-element/major-element ratios suggests that, in these dolerites. Ni occupies Fe +2 sites, Co and Sc replace both Mg and Fe +2 Cr replaces Fe +3 ,V +4 replaces Ti, Ga replaces Al and Ba and Sr both replace Ca.

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