The middle crust and the lower crust is in the ductile field.
上地壳表现为脆性变形,中、下地壳为韧性的流动变形。
In lower crust, faults often consist of a series of secondary fractures.
发育于地壳浅层中的脆性断层常常由一系列次级小断层所构成。
The faulting might be attributed to the ascending lower crust-derived fluids after the Late Miocene epoch.
造成断裂分期活动的原因是藏东地区下地壳流体的存在。
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