Moho

Moho has inner structure and can be found all over the continent.

莫霍面几乎遍布全国，它具有内部结构。

Three deep faults cutting the Moho discontinuity are also exhibited.

在深部可能有三个错断莫霍面的断裂带。

We pick up the instantaneous information of Moho phase in typical segment of the profile.

对典型剖面段的莫霍面震相进行瞬时信息的提取。

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。

Using gravitational and magnetic data of the area we calculated Moho and Courier interfaces.

根据研究区的重磁资料计算了该区莫霍、居里界面深度与分布。