1.
Applications of Seismic Surface Waves in the Study of Structures of the Crust and Upper Mantle (An Overview)
地震面波在研究地壳上地幔构造中的应用(综述)
2.
STUDY ON CRUST AND UPPER MANTLE STRUCTURE IN NORTH HENAN AND ITS SURROUNDINGS
豫北及其外围地区地壳上地幔结构研究
3.
PRIMARY STUDY OF CRUSTAL AND UPPER MANTLE VELOCITY STRUCTURE OF SICHUAN PROVINCE
四川地区地壳上地幔速度结构的初步研究
4.
A Seismic Tomography Study on Crust and Upper-mantle Structure Beneath the North-South Zone in China;
南北带地壳上地幔结构的层析成像研究
5.
Surface Wave Tomography in China and Adjacent Areas;
中国及邻区地壳上地幔面波频散层析成像
6.
The Seismic Tomography on the Velocity Structure of the Crust and Upper Mantle in the Northeastern Margin of the Qinghai-Tibetn Plateau
青藏高原东北缘地壳上地幔速度结构的地震层析成像研究
7.
THE CHARACTERISTICS OF THE ELECTRICAL STRUCTURE OF THE CRUST AND UPPER MANTLE IN THE REGION OF THE KUNLUN AND THE KARAKORUM MOUNTAINS
昆仑山脉和喀喇昆仑山脉地区的地壳上地幔电性结构特征
8.
3-D Velocity Structure of the Crust and Upper Mantle in Tibet and Its Geodynamic Effect;
青藏高原地壳上地幔三维速度结构及其地球动力学意义
9.
P wave velocity structure in the crust and upper mantle beneath northeastern South China Sea and surrounding regions
南海东北部及其邻近地区地壳上地幔P波速度结构
10.
The results show that the crust and upper mantle structures present obvious lateral and vertical inhomogeneity.
结果表明,地壳上地幔结构在纵向和横向上具有明显的不均匀性.
11.
In studying the structures of the crust and the upper mantle from refractions, the Tau method provides a new and effective approach.
在利用迥折波研究地壳上地幔构造时,τ是一种新的有效反演方法。
12.
STUDYING THE STRUCTURE OF CRUST AND UPPER MANTLE IN EAST ASIA AND WEST PACIFIC MARGINAL SEA BY RAYLEIGH SURFACE WAVE
用瑞利面波研究东亚及西太平洋地壳上地幔三维结构
13.
Surface Wave Tomography of the Crust and upper Mantle in Sichuan-Yunnan Region;
川滇地区地壳及上地幔结构面波层析成像
14.
Scientists call this layer of crust and upper mantle the lithosphere.
科学家称这层地壳和上部地幔为岩石圈。
15.
Electrical Structure Study of the Crust-upper Mantle in Dabie-Sulu Orogen
大别—苏鲁造山带地壳—上地幔电性结构研究
16.
The upwelling of the mantal substance along fractured zones may be the reason causing the abnormal crust and mantal structure.
地幔物质沿断裂带上涌，可能是形成异常壳幔结构的原因。
17.
In east pacific, however, the subduction direction of the subducting plate is the same as that of the flow of the mantle, so the current dip angle of the Benioff zone will be larger than the initial dip angle.
对地幔而言 ,则是地幔相对于地壳的东向流动。
18.
Like the earth, the moon is in layers, with a crust on the outside and a deep mantle below.
如同地球一样，月球上有地层，表面是一层地壳，其下是很深的地幔。