1·Fault gouge is an important factor which influences fault movement.
断层活动起着至关重要的作用。
2·Fault rocks with a random fabric include fault breccia, fault gouge, pseudotachylyte and cataclastic rocks.
具有紊乱组构的断层岩包括断层角砾岩、断层泥、假玄武玻璃以及碎裂岩。
3·Dating of fault gouge is now a common method for evaluation of faults activity, one of the quantitative methods.
目前，对于断层活动性评价较常用的方法就是有关断层样品的年龄测试，这是比较直观的定量方法之一。
4·The meaning and the method of study on mechanical properties of fault gouge has been described simply in this paper.
本文简要地叙述了研究断层泥力学性质的意义和方法。
5·The fractal dimension value is also relative with parent rock, thickness, structural position and clay content of the fault gouge.
分维值还与断层泥的母岩、厚度、粘土矿物含量和所处的断裂部位等相关。
6·In this paper, characteristics of neogenic clay minerals and micro-surface texture of quartz fragment in fault gouge are discussed.
本文主要研究断层泥中新生的粘土矿物特征，并研究断层泥中石英碎砾表面溶蚀的显微形貌结构特征。
7·The results show that (1)this fault zone can be divided into north, middle and south three segments based on the characteristics of the fabric from fault gouge.
结果表明：（1）根据断层泥组构特征，六盘山东麓断裂可划分为北、中、南3段，这与前人宏观分段结果相一致；
8·The first drilling hole of the Wenchuan earthquake fault science drilling project (WFSD-1) experienced up to more than 30 meters of the fault gouge drilling process.
汶川地震断裂带科学钻探项目一号孔(WFSD - 1)钻遇了30多米的断层泥。
9·In this paper the experimental results of mechanical properties of gouge of Yishu Fault-an important fault in North China-are reported.
本文介绍了华北的一条重要断裂-沂沭断裂的断层泥力学性质的实验研究结果。
10·The fault exists obviously in three bands: cataclasite concentrated joint band, worn braciation shearing rotation band and gouge partial pressure solution band.
断层岩在平面上分带特征明显，可划分为碎裂岩-节理密集带，磨砾岩-剪切旋转带和断层泥-局部压溶带等三个带。