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
参考文献
相似文献
引证文献
引用本文
葉良輔;.1925. THE MESOZOIC STRATIGRAPHY OF THE YANGTZE GORGES.[J]. ACTA GEOLOGICA SINICA(English edition),4(2):121~127