摘要
根据秦岭造山带郯庐断裂以东部分（本文称东秦岭造山带）的地质和地球物理特征，对东秦岭造山带的形成过程作了新的探索．并用新的造山作用模式解释了下扬子地区的性质、郯庐断裂为何至大别山南缘突然中止以及秦岭造山带为何被一分为二等重要问题．
Based on the geologic and geophysic data of east Qinling orogenic belt and surface geological observation, the orogcnsis of east Qinling orogenic belt that is in eastern part of Tanlu fault is studied in the paper. The new model explains well the tectonic characteristics and why Tanlu fault ends abruptly at the southern margin of Dabie Shan metamorphic complex and why Qinling oroganic belt was divided into two partS by Tanlu fault.
出处
《同济大学学报（自然科学版）》
EI
CAS
CSCD
北大核心
1997年第1期77-81,共5页
Journal of Tongji University:Natural Science
基金
国家自然科学基金
关键词
东秦岭造山带
下扬子地块
郯庐断裂
造山作用
East Qinling orogenic belt
Lower Yangtze massif
Tanlu fault
Orogensis
