1、Moho has inner structure and can be found all over the continent.
莫霍面幾乎遍布全國，它具有內(nèi)部結(jié)構(gòu)。

2、Using gravitational and magnetic data of the area we calculated Moho and Courier interfaces.
根據(jù)研究區(qū)的重磁資料計算了該區(qū)莫霍、居里界面深度與分布。

3、The Qinling Moho zone formed after crust balance play so-called "the foot of a hill" role.
受地殼均衡作用的影響，已形成的秦嶺殼幔過渡帶起到了通常所說的“山根”作用。

4、Even further south, reflections from 35 km depth may correspond to the Moho of peninsular India.
再往南從35公里深度來的反射波是來自印度半島的莫霍界面。

5、Three deep faults cutting the Moho discontinuity are also exhibited.
在深部可能有三個錯斷莫霍面的斷裂帶。

6、RESEARCH OF MOHO BASIC FEATURES ON EASTERN QINLING DEEP SEISMIC PROFILE
東秦嶺深地震剖面上莫霍基本特征的研究

7、Even further south, reflections from 35km depth may correspond to the Moho of peninsular India.
再往南從35公里深度來的反射波是來自印度半島的莫霍界面。

8、We pick up the instantaneous information of Moho phase in typical segment of the profile.
對典型剖面段的莫霍面震相進行瞬時信息的提取。