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地壳各部分所发生的一切形变都是地应力作用的反映。在组成地壳的岩石矿物内也必然保存着长期地应力作用的痕迹。应力作用可以影响到矿物的晶格内部,例如使晶格发生位错。地质学的深入发展,要求进一步解决怎样通过组成地壳的岩石内留下的变形迹象
All the deformations in various parts of the crust are a reflection of the role of geostress. The rocks and minerals that make up the crust also inevitably preserve traces of long-term stress. Stress can affect the interior of the crystal lattice of minerals, for example dislocating the lattice. The in-depth development of geology calls for further resolution of the signs of deformation left in the rocks that make up the crust