摘要
一 解放以前,涉及秦岭两側构造地貌与河流发育的論述頗多,較著名者有:李連捷、赵亚曾与黄汲清、李承三等、王德基、冯景兰等。解放以后,随着国民經济的发展和水利建設的跃进,对秦岭两側地貌也有了更多的討論。
It is necessary to investigate and make clear the development of the streams in the Chinling district in relation to block-faulting of the"Basin-Range"type for the purpose of hydraulic constructions.The geologic structures of the ranges of Chinling are distinctly characterized by neotectonic block-faulting.Despite of the folding and metamorphism of the mountain belt in the earlier geologic periods,it is found that there had been in Chinling districts gentle flexuring features during the cycle of Yenshan movements,and block-faulting were began during the period of Himalayan movements.
出处
《地质学报》
1964年第4期405-417,共13页
Acta Geologica Sinica
