摘要
文章对北京西山一带,中元古界至下古生界沉积岩系中的粘塑性流动变型构造,从实际资料出发,论证其成因类型,并进而提出固态流变构造与同沉积构造的区别标志。
In this paper the attributes of the rheomorphic structures are for the first time dealt with in details and the general features of synsedimentary deforma- tion structures both at home and abroad are summarized systematically.Thro- ugh comparison,nine.applicable criteria for distinguishing rheomorphic stru- ctures from synsedimentary deformation structures are proposed.
出处
《中国区域地质》
CSCD
1989年第1期86-94,共9页
Regional Geology of China