Along the north flank of the Yellow River delta the older hard-rock formations have been thrown into long parallel folds by Mesozoic deformation. Under later Tertiary erosion this structure has determined the trend of the
Abstract:
Along the north flank of the Yellow River delta the older hard-rock formations have been thrown into long parallel folds by Mesozoic deformation. Under later Tertiary erosion this structure has determined the trend of the
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G. B. BARBOUR.1926. DEPOSIT AND EROSION IN THE HUAI-LAI BASIN AND THEIR BEARING ON THE PLEISTOCENE HISTORY OF NORTH CHINA.[J].地质学报,(1). G. B. BARBOUR.1926.[J]. Acta Geologica Sinica,(1).
