An inversion of velocity structure of crust and upper mantle by using converted PS wave and multiwave PPP etc, is reported in this paper.
本文是研究利用天然地震PS转换波及PPP等二次波到时资料反演地壳上地幔速度结构的尝试。
There is close relation between loading tidal correction and structure of crust and upper mantle.
负荷潮汐改正与地壳上地幔结构有密切关系，主要原因是负荷潮汐取决于高阶勒夫数。
The results show electric property structure of the crust and upper mantle clearly.
揭示了该剖面地壳上地幔电性结构特征，并进行了划分。
Based on the data of focal mechanism solutions, and velocity structure in the crust and upper mantle, we have investigated the recent tectonics with relation to the origin of the plateau.
本文以震源机制、地震地质、地壳和上地幔速度结构等资料为基础，研究了与青藏高原成因有关的现代构造问题。
The S wave velocity structure is inferred from the receiver function for the crust and upper mantle of the Wudalianchi volcano area.
可以推断，从接收器功能的S波速度结构 五大连池火山区地壳和上地幔的。
This paper introduces a result of 2-d density structure of the crust and upper mantle in Luyang-Haicheng-Donggou DSS profile using the DSS data obtained from the profile.
本文介绍了应用闾阳—海城—东沟剖面深地震测深资料研究该剖面地壳与上地幔二维密度结构的结果。
The relation between seismic anisotropy in crust and in upper mantle can show the geodynamic specialties of shallow and deep structure, and can hint information about geodynamic mechanism;
上地幔介质各向异性与地壳介质各向异性的关系能够反应区域浅部与深部介质动力学特征，并暗含区域动力机制信息；
The relation between seismic anisotropy in crust and in upper mantle can show the geodynamic specialties of shallow and deep structure, and can hint information about geodynamic mechanism;
上地幔介质各向异性与地壳介质各向异性的关系能够反应区域浅部与深部介质动力学特征，并暗含区域动力机制信息；
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