摘要
The characteristics of slope break during depression stage in the Songliao Basin of NE China are analyzed. It is indicated that double flexure slope breaks extend in a circle across the basin.One is nominated the inner slope break,and the other is the external slope break. Under different regional stress field,the control
作者
Xuebin Du~1,Xinong Xie~1,Jianye Ren~1,Yongchao Lu~1,Tao Cheng~2,Ming Su~1 1.Faculty of Earth Resources,China University of Geosciences(Wuhan),Wuhan 430074,China. 2.Beijing Research Center of CNOOC,Beijing 100027,China
出处
《地学前缘》
EI
CAS
CSCD
北大核心
2009年第S1期149-150,共2页
Earth Science Frontiers