Effect of Cenozoic Altun Fault Activity on Structural Deformation in Surrounding Basins
详细信息   
摘要
There are Jiuquan Basin, Qaidam Basin and Tarim Basin in the south-north sides of Altun fault belt. This paper proposes the stress-strain theoretical model of “active wall plus passive wall” and presents a rational interpretation for such structural differences between the north and south sides. It is considered that the geological body of the southern side of Altun fault belt is directly affected by the India-Eurasia Plate, being regarded as the active wall, while that of the north side is affected by NW component of remote stress, being as the passive wall.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700