摘要
南昆仑造山带西段发育逆冲推覆构造、平行走滑构造、地垒—地堑构造和阿尔卑斯式褶皱、侏罗山式褶皱,前两类构造尚有韧性剪切带伴生;其构造组合在平面上具有内带—外带—前陆带明显的分带性,且形成了逆冲推覆构造—平行走滑构造—地垒—地堑构造的构造序列。
Lied at the western section of south Kunlun orogenic zone, there developed with the thrust nappe structure, parallel glide structure, horst-crabon structure, Alpine-type folds and Jurassic folds, the former two sorts of structures still have been accompanied by ductile shearing belts; Horizontally the structural combination is displayed with obvious zoning of inner zone, off zone and fore zone, in addition forming structural sequence of the thrust nappe structure, parallel glide structure, horst-crabon structure.
出处
《贵州地质》
2004年第1期24-29,共6页
Guizhou Geology
基金
地调项目:属1:25万奥依亚依拉克
羊湖幅区调项目成果。
