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 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.
这些构造构成了一个在成因上与拆离断层形成有关的伸展构造体系。
These structures form an extensional tectonic system that is genetically related to the formation of the detachment fault.
武功山伸展拆离滑覆构造主要形成时期在晚三叠世之前，但晚三叠世之后仍有活动。
The gliding nappe structure was mainly formed before the late Triassicera, but it was still mobilizing after the late Triassic era.
区内主要滑动面有三个，主要伸展型滑脱拆离断裂有三条，并具有复杂的构造组合。
With a complex tectonic assemblage, there are three principal slip planes and three main extensional decollement - decoupling faults in this area.
可划分为伸展变形、冲断褶皱变形、拆离滑脱变形等3种构造变形样式。
The deformation style includes 3 types: stretching deformation, thrust fold deformation and decoupling slip deformation.
伸展条件下的地壳拆离作用是岩石圈减薄的重要浅部构造响应。
Extensional crustal detachment is the most important tectonic response of lithosphere thinning.
武功山伸展拆离滑覆构造主要形成时期在晚三叠世之前，但晚三叠世之后仍有活动。
The gliding nappe structure was mainly formed before the late Triassicera, but it was still mobilizing after the late Triass…
武功山伸展拆离滑覆构造主要形成时期在晚三叠世之前，但晚三叠世之后仍有活动。
The gliding nappe structure was mainly formed before the late Triassicera, but it was still mobilizing after the...
山西高原内部中新生代拆离构造特征与太行山前类似，伸展构造以拉分断陷为主。
The extensional structures in Mesozoic-Cenozoic inside the Shanxi Plateau are mainly characteristic of pull-apart basin development, similar to the ones in front of the Taihang Mountains.
山西高原内部中新生代拆离构造特征与太行山前类似，伸展构造以拉分断陷为主。
The extensional structures in Mesozoic-Cenozoic inside the Shanxi Plateau are mainly characteristic of pull-apart basin development, similar to the ones in front of the Taihang Mountains.
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