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。
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。
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。
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。
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。
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。
The OBS has recorded Moho and other seismic waves, the sedimentary layer, the upper crust layer and the lower crust layer can be identified from it.
OBS记录到了包括莫霍面在内的地震波，可以识别地壳内沉积层、上地壳层、下地壳层等多个层位的折射波地震相。
The variable density model is more suitable for inversion of Moho depths structures than constant density model by comparison of Moho depth from seismic inversion.
通过常密度模型、变密度模型及地震反演得到的莫霍面的比较，证实变密度模型更适合于莫霍面结构的反演。
The steeply sloped Moho belts (and other interfaces) and mid-crustal soften layer could be considered as a deep structural mark for being pregnant with earthquakes.
深部构造(M面和其它界面)的剧变带和中地壳柔层可力判别地震孕育的深部标志。
Strong earthquakes often occur in regions that are located between upheaval and subsidence of the Moho surface or density reduction and density increase of the interface.
地震往往发生在莫霍面隆起区与沉降区、密度减小区与增长区的过渡地带。
Sedimentary basin forming dynamics system is the macroevolution and correlation of the sedimentary basin, the mantle, the asthenosphere, the lithosphere, and Moho discontinuity.
成盆动力学系统是一个包括沉积盆地及其下的地幔、软流圈、岩石圈和莫霍面等不同地质单元的宏观变化和相互制约的过程。
It is controlled Chiefly by the lithospheric thickness and the Moho depth, and partly by the thickness of various tectonic layers, physical properties and magmatic activity, etc.
各地区各构造层段具有不同的热结构特征和热演化史，它总体上受控于岩石圈厚度及莫霍面的理深，局部受控于各构造层的厚度、物性特征及岩浆活动等因素。
Subtracting the gravity anomalies caused by density anomalies from the observed Bouguer anomalies, we inversed the depth of Moho of northwestern China by using the residual anomalies.
在从观测布格重力异常中扣除上述密度异常引起的重力异常后的数据基础上，直接反演了中国西北区域莫霍界面的深度。
Perhaps there are some tension fractures in it. 4. The complex folds in the upper palaeozoic, the volcano and the seismic zones may be related to the undulation of Moho discontinuity.
苏南的上古生代紧密褶皱、火山与岩浆活动以及二个地震活动带的存在，均与莫氏面的起伏有关。
Moho depth distribution and crustal deformation pattern between different sub-blocks in Sichuan-Yunnan region are presented here based on the studies of the gravity field characteristics.
对川滇地区重力场特征进行了研究，获得了研究区内地壳厚度分布及变形特征。
Using gravity data the depths of Moho and Conrad discontinuities in North China region are calculated and thus the basic configuration of crustal structure in this region can be determined.
本文利用重力资料计算了华北地区康氏面和莫氏面的深度，从而得出了这一地区地壳结构的基本形态。
The mantle convection is the primary driving force for the formation and evolution of sedimentary basins, and manifested in the position of the asthenosphere, Moho discontinuity and mantle plume.
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。
The mantle convection is the primary driving force for the formation and evolution of sedimentary basins, and manifested in the position of the asthenosphere, Moho discontinuity and mantle plume.
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。
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