地貌沉积学方法在活断层研究中的应用

Summary on the Sedimentary-geomorphologic Method Used in the Study of Active Faults

摘要:

地貌沉积学方法是研究活动断层运动规律的有效方法之一。综合大量已有研究成果,本文从活断层垂直运动、水平运动及垂直-水平组合性运动特征等方面对地貌沉积学原理在目前活断层研究工作中的应用及进展进行了综述;并探讨了今后地貌沉积学方法在活断层研究中需关注的一些关键技术。

Abstract:

Sedimentary-geomorphologic method is an effective way to study the kinematic laws of active fault. From the great amount of existing researchs, the main contents and progress in the research are summarized in three aspects as kinematic characteristics of active fault with vertical movement, horizontal movement and the vertical-horizontal eompositing movement. Some key techniques could be used in the sedimentary-geomorphologic method in active fault research in future are discussed also.