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应力场的分析表明，劈理构造由近南北向的地壳水平挤压应力作用形成。
The stress field analysis showed that the cleavages formed under horizontal, S-N trending compressive stress.
由活动断裂所构成的一系列医陷谷地显示了该区新构造应力为近南北向的水平挤压应力。
A series of compressional depressed valleys formed by active faults show that the neotectonic stress field in the area is controlled by horizontal compressional stress.
由活动断裂所构成的一系列医陷谷地显示了该区新构造应力为近南北向的水平挤压应力。
Few faults had sinistral activities. A series of compressional depressed valleys formed by active faults show that the neotectonic stress field in...
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