地质通报2016，Vol.35Issue(4)：503-518,16.
中蒙边界中西段地层划分与对比
The division and correlation of strata in the mid-western part of Sino-Mongolian border area
摘要
Abstract
In the Sino-Mongolian border area, the Early Precambrian-Cenozoic strata are widely distributed but assigned to different stratigraphic classification systems. On the basis of lithostratigraphy and tectonic evolution, the authors hold that, from Altay of China to Gobi-Tianshan of Mongolia, the strata are continuous and can be divided in unified way. With the Ertysh-Burgen fracture, Karamic fracture, Borzon fracture and East Mongolia-Diebusigo fracture as the boundary, the strata in mid-western border area can be divided into three parts, i.e., Altay zone, Junggar-Gobi Altay zone and Beishan-Gobi Tianshan zone. In this paper, the unified di⁃vision and correlation of strata in this area were carried out.关键词
中蒙边界/中西段/地层划分/特征对比Key words
Sino-Mongolian border area/mid-western part/stratigraphic division/feature comparison分类
天文与地球科学引用本文复制引用
付超,李俊建,唐文龙,张锋,任军平,党智财,Orolmaa Demberel,Tumurtogoo Onongyn..中蒙边界中西段地层划分与对比[J].地质通报,2016,35(4):503-518,16.基金项目
中国地质调查局项目（编号1212010561510、1212010811061、1212011120330、12120114001201、1212010781028、1212011085488）、国土资源公益性行业科研专项（编号200811010）和国家国际科技合作项目 （）
