断裂构造是一种基本的构造型式。
区域构造格局控制成矿带的分布，不同构造单元具有不同的控矿构造型式。
Regional structures control the distribution of gold metallogenic belts, and different structural units control different types of ore-controlling structures.
会聚构造型式以对冲式及叠覆式为主要类型，形成时期在晚始新世—渐新世。
The main patterns of the convergent structure are the ramp type and the superimposed one. And their forming periods are Late Eocene Oligoecne.
地震在空间上的分布和在时间上的活动规律受这一构造型式及其应力状态的控制。
The earthquake distribution in time and space is controlled by the tectonic pattern and relevant stress states.
本文根据野外调查和原地应力测量资料，讨论了滇西北地震活动区的活动构造型式和现今应力状态。
The active tectonic pattern and recent stress state in the seismic region of NW Yunnan province are discussed on the basis of field observation and in-situ stress measurements.
本文根据野外调查和原地应力测量资料，讨论了滇西北地震活动区的活动构造型式和现今应力状态。
The active tectonic pattern and recent stress state in the seismic region of NW Yunnan province are discussed on the basis of field observation and in-situ stress measurements. Data.
该模型还可计算不同冰面温度和换热条件下所需的制冷剂温度，分析不同的冰场地下构造型式对温度场的影响情况。
The effect of rink structure on temperature field is also discussed, which will help designers to adopt new underground structure type.
该模型还可计算不同冰面温度和换热条件下所需的制冷剂温度，分析不同的冰场地下构造型式对温度场的影响情况。
The effect of rink structure on temperature field is also discussed, which will help designers to adopt new underground structure type.
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