| 释义 |
Mo·ho 英ˈməʊˌhəʊ美ˈmoˌhoAHDmōʹhō' BNC¹⁴⁴⁶⁶⁴⁺³
基本英英近义反义例句例句
moho 地壳与地幔间的界限
Noun:
the boundary between the Earth's crust and the underlying mantle;the Mohorovicic discontinuity averages 5 miles down under oceans and 20 miles down under continents 近义词 mohorovicic discontinuity莫霍间断面,莫霍不连续面…
TheMohoupheaves 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 theMohoof 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 ofMohoand 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。
Mohodepth 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 QinlingMohozone 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。
There exists a deep fault cutting theMohoor a anomalous deep structure in the epicenter region.在震区的下方存在著M面断裂或构造异常带。 In this paper, PS reflection was used to determine the depth and fluctuation of Moho discontinuity in the local region of the north side of the Yarlung Zangbo River.
本文利用 PS反射波探测了雅鲁藏布江北侧局部地区莫霍面的深度和起伏。 http://dj.iciba.com
So the complex structure and morphology of the Moho are the deep tectonic background of Xingtai seismic area.
复杂的莫霍面结构和形态是邢台地震区的深部构造背景。 cnki
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。 cnki
The relation between Mesozoic basement and Moho depth is positive, but the Cenozoic basement is in negative correlation with Moho depth.
中生代沉积基底与莫霍面呈正相关，而新生代沉积基底则与莫霍面呈明显的镜像关系。 cnki
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。 cnki
The sedimentary basement and Moho basement are important interfaces in the crust of ocean, and their forms and depths have been extensively studied.
海洋深部地壳结构研究，主要研究沉积基底面与莫霍面的形态与埋深。 cnki
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。 cnki
There are obvious differences about the Moho seismic event features of the plate of north China and Yangtze as well as Qinling orogenic belt appeared on Eastern Qinling deep seismic profile.
东秦岭深地震剖面上反映的华北、秦岭和扬子莫霍地震波组的特征具有明显差异。 cnki
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。 cnki
As a geophysical term, Moho discontinuity has its own inherent definitions, it may not be the same with isostatic surface generally suggested.
作为地球物理术语，莫霍不连续面有它自己的特定定义，它不一定和通常所说的均衡面是一个东西。 cnki
Characteristics of Moho is significant to deep structures in East China 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。 cnki
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。 cnki
Even further south, reflections from35km 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。 cnki
Finally, the connection of the form of Moho discontinuity with magmatic intrusion and distribution of mineral resources is discussed.
最后，探讨了莫霍面形态与岩浆岩侵入体、矿产间的联系。 cnki
In this paper, the PKP residual variations along the central Tibetan profile is analysed and found that Moho steps are the common features beneath Tibetan Plateau.
本文分析了远震PKP走时残差沿高原中部剖面的变化，发现莫霍面的断错在整个高原是普遍存在的； cagsbulletin
Inversion shows Moho discontinuity depth increase from land to sea and the distribution of continental crust, extensional crust, transitional crust and oceanic crust.
反演得到的莫霍面总体趋势由陆向洋抬升，反映陆壳、拉伸陆壳、过渡壳、洋壳的分布。 cnki
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。 cnki
On the basis of recent data of gravity, the Bouguer anomalies of Moho discontinuity were divided by canonical filtering of frequency domain.
利用最新重力资料，采用频率域正则化滤波分离莫霍面的布格异常； cnki
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。 cnki
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。 dictall
The deep geological processes such as the tilting and subsiding of Moho discontinuity, large-scaled deepmagmatism and deep faulting are main controlling factors for uranium metallogenesis;
深部地质作用如莫霍面的起伏、深部大规模的岩浆活动和深断裂作用是铀成矿的重要控制因素； cnki
The results indicate that the three- instantaneous information can improve the interpretation on characteristics of Moho using the original section.
结果表明，利用三瞬信息可以补充原始剖面上莫霍面的解释。 cnki
The variable density model is more suitable for inversion with Moho depths structures than constant density model by comparison of Moho depth from seismic inversion.
通过对常密度模型、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。 cnki
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。 cnki
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。 cnki
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。 cnki
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。 cnki
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。 cnki |