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Information Journal Paper

Title

PETROLOGY OF SHOSHONITIC LAVAS IN SOUTH OF ASHIN VILLAGE (EAST OF ISFAHAN)

Pages

 Start Page 89 | End Page 98

Abstract

 Eocene felsic to basic SHOSHONITIC LAVAS are located in the Uromia-Dokhtoar structural zone. These association rocks are Absarokite, shoshonite, banakite and toscanite. PETROLOGY and geochemistery evidence indicate that the lavas were formed by fractionation of alkali basalt magma combined with assimilation of continental crust. Eruption of alkali basalt correlates with a POSTCOLLISIONAL ARC.

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