Mohos

基本解释

The Moho upheaves at the basin center and dips toward the basin edge.
莫霍面形态中部上隆，盆地南北边缘分别向南、北加深；
Even further south, reflections from 35km depth may correspond to the Moho of peninsular India.
再往南从35公里深度来的反射波是来自印度半岛的莫霍界面.
The rise of the asthenosphere,the position of Moho and mantle plume are the indication of the mantle convection.
软流圈上涌高度、莫霍面或地幔羽的位置是地幔对流的具体的表现。
Moho depth increases from 33 to 34 km on east side and from 36 to 38 km on the west side.
断裂带东侧莫霍面埋深浅;大约为33~34km; 西侧莫霍面埋深明显增加;达到36~38km.
The Qinling Moho zone formed after crust balance play so-called “the foot of a hill” role.
受地壳均衡作用的影响，已形成的秦岭壳幔过渡带起到了通常所说的“山根”作用。