摘要
通过对内蒙古中部地区苏尼特左旗等８幅图（约３０００ｋｍ２）１∶５万区域地质调查，发现了交其尔构造带。该构造带由浅部的逆冲推覆断裂与深部的韧性剪切带上、下叠置而成。
The Jiaoqier complex structural belt in the central Inner Mongolia was discovered in the 1∶50000 regional geological survey, which is composed of the thrusting nappe structure near surface and the ductile shear zone in depth.
出处
《地质与勘探》
CAS
CSCD
北大核心
1998年第5期18-22,共5页
Geology and Exploration
关键词
内蒙古
逆冲推覆断裂
韧性剪切带
交其尔构造带
central Inner Mongolia, Jiaoqier, thrusting nappe fault, ductile shear zone
