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。

youdao

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。

youdao