Abstract
ABSTRACT Cyclic repetition of limestone and dolomite was studied in a railroad cut near Charlton, Maryland. 35 cycles were recognized, each composed of a basal dolomite member and an upper limestone member. Field and petrographic evidence suggests a primary origin for the dolomites in the section studied. The cyclic repetition of dolomite and limestone, it appears, was due to tectonism.
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Schedule a callMore From: Journal of sedimentary research. Section A, Sedimentary petrology and processes : an international journal of SEPM (Society for Sedimentary Geology)
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