摘要
通过1:5万区调工作,在巢湖一带发现了多层次推覆构造。木文结合区域地质情况,对多层次推覆构造及形成的主要条件等作一介绍。
Polylevel nappe structures have been recognized in the Chaohu area, Anhui Province, according to a study, analysis and comparison of a large amount of sedimentological, paleontological, geophysical and geochemical data. Based on the overlapping relationship, they may be divided into three sheets: the upper nappe, middle nappe (Yinping allochthon) and lower nappe. Analyses of tectonic environments and stratigraphy indicate that these nappes resulted from lateral compression and gravity gliding.
出处
《中国区域地质》
CSCD
1989年第4期324-331,35,共8页
Regional Geology of China
