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.
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