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走滑运动与调整断层
引用本文:李万程.走滑运动与调整断层[J].中国煤田地质,1995,7(3):1-5.
作者姓名:李万程
作者单位:河南煤田地质局
摘    要:走滑运动是指沿直立的断面作走向滑移的断裂运动。走滑断层可分为两种:一是单剪性质的走滑断层,按习惯称为平移断层;二是作为挤压带、伸展带、重力滑动带的侧向连系和调整的走滑断层,建议称为调整断层。建立调整断层的目的,在于拓宽对走滑运动内涵的认识,增强对走滑构造多样性的理解。

关 键 词:走滑运动,侧向构造,调整断层

STRIKE-SLIP MOVEMENT AND REAKJUST FAULT
Li Wancheng.STRIKE-SLIP MOVEMENT AND REAKJUST FAULT[J].Coal Geology of China,1995,7(3):1-5.
Authors:Li Wancheng
Abstract:The strike-slip movement remarks a fault movement has a shove along avertical plane of fault.There are two kinds of strike-slip fauIt:1)simple shear strike-slipfault,has long been known as parallel displacement fault;2) readjust fault is a fault thatlinks compressional,extensional,gravitational sliding belts laterally and readjusts the relationbetween them. The purpose of to advance the readjust fault is the author hopes to broadenthe understanding of the intention of strike-slip movement,helps to find out the diversity ofstrike-slip structures.
Keywords:Strike-slip movement  Lateral structure  Readjust fault
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