摘要
临汾盆地第四纪断层非常发育，按其走向可分为ＮＮＥ、ＮＥ、ＮＷ和ＥＷ向几组。本文指出第四纪期间，这些断层活动的表现形式为河流现代过程的变异，谷沟形态异常，或使晚新生代沉积相带迁移和晚更新世以来的地层错断等。
The Quaternary faults in Linfen basin is very well developed,according to the strike,it can be dividedinto 4 groups of NNE, NE, NW and EW trending.The paper suggests that in Quaternary period,the exhibi-tion types of the faulting are the variation of the present day process of the river, the anomaly of the valleyand trench the migration of the Late Cenzoic Sedimentary facies zone and the stratigraphical displacementsince Late Pleistocene Epoch.
出处
《山西地震》
1995年第3期54-59,共6页
Earthquake Research in Shanxi
