The existence of embedded high velocity thin layers in lower lithosphere may be of significance in the evolution of the lithosphere.
岩石圈中薄层的存在对于岩石圈的演化过程具有重要的意义。
The experiments also show that the origin of large scale compressional basins are associated with the existence of stable blocks in the lower lithosphere.
实验还表明，大型压性盆地的形成与岩石圈下层稳定块体的存在有关。
It is tentatively suggested that the lower lithosphere MORB-OIB mantle is recently accreted since the paleo-lithosphere mantle was replaced by the abnormal asthenosphere.
我们初步认为，该区深部岩石圈MORB - OIB地幔可能是软流圈置换古岩石圈地幔而增生形成的。
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