全部

1·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。

2·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。

3·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。

4·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。

5·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。

6·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。

7·Even further south, reflections from 35 km 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。

8·Moho depth within the crust and upper mantle, high conductivity layer depth and heat flow values have close relations.

通过对该区的研究发现，在地壳和上地幔中莫霍面埋深、高导层埋深和热流值之间存在着密切的联系。

9·The residual gravity anomaly was mainly produced by rolling basement of the basin and the regional gravity anomaly by the Moho rolling.

推断引起剩余重力异常的主要原因是盆地基底的起伏，引起区域重力异常的主要原因是莫霍面起伏。

10·Characteristics of Moho is significant to deep structures in East Sea because Moho is important density inference between Crust and Mantle.

莫霍面是地壳和上地幔的分界面，是个重要的密度界面，东海莫霍面的展布特征，对于研究东海深部构造具有重要意义。