摘要
将理论分析与野外资料解释相结合,对断层判别依据作进一步讨论。通过对下辽河盆地和辽西、内蒙地区部分浅部断层数字化记录资料的正、反演计算,作了运动学特征和动力学特征分析,得出有益结论。
The identification basis of shallow faults has been made a discussion by combining theoretical analysis with practical interpretation in this paper.Having made theoretical caculation and inversion of the digitalized records of some shallow faults in lower Liao River Basin,west Liaoning and Nei Mongol,kinematic and dynamic characteristics haue bern studied,and it is significant to obtain some conclussions in the study. Conclusions have been obtained.
出处
《东北地震研究》
1998年第1期52-60,共9页
Seismological Research of Northeast China