The third phase deformation is normal fault that developed along the formation interface from different times or the same stratum with different lithology in the basin.
第三期变形为沿盆地内不同时代地层界面或同一地层不同岩性界面发育的伸展拆离构造；
The interface energy that exists between the sheets could be minimized by the grain boundaries by the formation of dislocations or pairs of rings.
而不同的石墨烯面之间存在的表面能可以通过在晶界处形成空位或者位错环而得到降低。
Calculations demonstrate the formation of facets and anisotropic undercooling distribution along the interface.
计算结果显示了小面的形成和界面上各向异性的过冷度分布。
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