现今地温场主要受岩石圈厚度、构造特征和地下水活动的影响。
The present geothermal field is controlled by thickness of lithosphere, structural features as well as groundwater activity.
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.
黑孜尔断裂现今活动方式继承了新构造运动以来的运动特点。
The present motion mode of Heizir fault inherits the characteristic of new tectonic motion.
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