The Hangnest Dolerite Sill, S.A

Abstract
A 500 ft. sill of dolerite from Hangnest in the Calvinia division of the Cape Province (South Africa) exemplifies very clearly two well-marked features of the thicker Karroo sills:—(1) Very slight amount of crystallization-differentiation.(2) Marked tendency to mobilize and react with the associated shales and siltstones.A petrological and chemical study of this sill is given and the mechanism of the various processes discussed.

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