1.
PRELIMINARY STUDY ON THE LATERAL VELOCITY VARIATION OF THE UPPER MANTLE IN NORTHERN XINJIANG AND ITS ADJOINING REGIONS
北疆上地幔波速特征侧向变化的探讨
2.
Mantle surface wave of the great Sumatra-Andaman earthquake recorded by the Global Seismograph Network
全球地震台网记录苏门答腊-安达曼地震的地幔波
3.
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)
4.
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
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.
CHARACTERISTICS OF SEISMIC VELOCITY STRUCTURE OF THE CRUST AND UPPER MANTLE AND MOHO DISCONTINUITY IN GULEI-SHICHENG AREA
古雷—石城地区地壳与上地幔地震波速度结构及莫霍面特征
7.
Seismic converted wave is one of methods of explorating earth crust and upper mantle.
地震转换波法是探测地壳与上地幔构造的方法之一.
8.
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
9.
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。
10.
LOVE WAVE GROUP DISPERSION AND THREE DIMENSIONAL STRUCTURE OF THE PACIFIC CRUST AND UPPER MANTLE
勒夫波群速度频散与太平洋地壳及上地幔三维构造
11.
Shear Wave Velocity Structures in Crust and Mantle of North China and Study on the Relationship with Geological Evolution Since Late Cenozoic
华北地区壳幔剪切波速度结构及与晚新生代地质演化关系研究
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.
Tomography for The 3-D S -Wave Quality Factor Q_B Structure of Crust and Upper Mantle in China;
中国大陆地壳上地幔S波品质因子三维层析成像
14.
The 3-D velocity structures of the Eurasian mantle based on the body wave tomography
利用体波层析成像技术研究欧亚及邻区地幔三维速度结构
15.
Tomography for the 3-D S-Wave Quality Factor Q_β Structure of Crust and upper Mantle in China and Adjacent Areas;
中国大陆及邻区上地幔S波品质因子三维层析成像
16.
High Resolution Body-Wave 3-D Tomography of Mantle of China and Adjacent Areas;
中国及邻区地幔三维结构高分辨率体波层析成像
17.
An ornamental hanging of rich fabric, as behind an altar.
幔布祭坛后面等地的幔布
18.
Therefore, the CMB is the beginning and the end of whole mantle convection.
因此,地幔底层既是全地幔对流的起点,又是全地幔对流的终点。