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.
就算这种愿景让科学实验室在原地停留几年，它当然仍得首先克服海森堡那个棘手的测量悖论。
If such a vision is to leave the science lab where it has been stuck for some years, it will of course still have to overcome Heisenberg's tricky measurement paradox first.
根据该区原地应力测量资料反演了区域应力场方向。
By inversion of the data of in-situ stress measurements the direction of regional stress has been obtained.
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