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含柯石英榴辉岩、高压片麻岩的五庙超高压变质岩与外围低压片麻岩以边冲断层呈构造侵位关系,而在其内部榴辉岩与高压片麻岩为非构造接触,并且发育有榴辉岩相静态重结晶构造以及在纯剪应力状态下的前角闪岩相变形构造D_1和在顶端指向NNW运动的单剪应力状态下的角闪岩相变形构造D_2。
The Wumiao UHP metamorphic rocks containing coesite eclogite and high-pressure gneiss are structurally emplaced with peripheral low-pressure gneisses in the thrust faults, whereas the eclogites and high-pressure gneiss in the interior are non-structural contacts , And the eclogitic recrystallization structure of eclogite facies and the amphibolite facies deformation structure D_2 in the pure shear stress state and the amphibolite facies deformation structure D_2 in the single shear stress state with the top pointing to the NNW movement are developed.