Paleocurrent analysis on the basal conglomerate of the model Changzhougou formation in Qian’an

Abstract

The paleoflow direction of the basal conglomerate of the Changzhougou formation is obtained by the paleocurrent analysis of certain sedimentary structures, and the ancient sedimentary environment of the Qian’an Region is determined by observing the psephicity and gradation of gravel in conglomerate. The results show that the paleoflow direction is from… (More)
DOI: 10.1007/s11859-016-1156-7

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