断层泥是断层活动的信息载体，其中的石英颗粒微形貌特征能够反映断层活动方式、期次和活动年代。
Gouge is an information carrier for fault activity. The motion mode and date of the fault activity can be identified by observation of micro-shape characteristics of quartz in the gouges.
在此基础上，根据已有理论结果和实际资料，对利用热释光方法断代及推测断层活动方式的可能性等问题进行了讨论。
Based on the result and the existing theory, the applicability of thermoluminescent method to dating the faulting and to determining the sliding mode along the fault is discussed.
断层泥是断层活动的信息载体，其中的石英颗粒微形貌特征能够反映断层活动年代、活动方式。
Gouge is an information carrier for fault activity, and the motion mode and date of the fault activity can be identified by observation of micro-shape characteristics of quartz in the gouges.
断层泥是断层活动的信息载体，其中的石英颗粒微形貌特征能够反映断层活动年代、活动方式。
Gouge is an information carrier for fault activity, and the motion mode and date of the fault activity can be identified by observation of micro-shape characteristics of quartz in the gouges.
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