地壳速度结构模型表明：塔里木盆地具有陆壳性质。
The crust velocity model of Tarim basin indicates its continental character.
用近震资料能得到在水平向和垂直向分辨率较高的地壳速度结构。
The better resolution in horizontal and vertical compenents for the crustal velocity structure can be obtained by using local earthquake data.
北京地区上地壳速度结构、断裂活动和物质性质三者之间存在密切关系。
There is a close relationship among velocity structure, active faults and upper crustal materials around Beijing area.
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。
An inversion of velocity structure of crust and upper mantle by using converted PS wave and multiwave PPP etc, is reported in this paper.
内地壳和上地幔S波速度结构与强震的关系和强震活动的深部背景进行了探讨。
Study to the relation between strong earthquakes and S-wave velocity structures in the crust and upper mantle in the studied area.
GABWIT是应用地震体波走时资料、遗传算法反演地壳三维速度结构的软件。
GABWIT is a software of inversion for 3d crustal velocity structure using seismic body travel time data and genetic algorithms.
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。
The S wave velocity structure is inferred from the receiver function for the crust and upper mantle of the Wudalianchi volcano area.
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。
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.
结果表明，该区地壳深部速度结构与构造在纵向和横向上具有明显的不均一性。
The results show strong vertical and lateral inhomogeneity in deep crust velocity structure and tectonics.
理论数值实验显示：在反演地壳S波速度结构时，SV分量接收函数比径向接收函数具有更好的收敛性。
The synthetic tests show that the convergence of SV-component receiver function inversion is faster than that of the radial receiver function inversion.
获得了该区地壳地一维速度结构，并讨论了解的分辨率。
The 1-d crustal velocity structure in this area is obtained and the resolution is also given.
层析成像结果较好地揭示了地壳内部、尤其是浅部地壳的横向速度变化。短周期的群速度分布同地表地质结构、地形密切相关；
The maps at short periods reveal an evident lateral heterogeneity in the crust of North-China, quite well in agreement with known geological and tectonic features.
层析成像结果较好地揭示了地壳内部、尤其是浅部地壳的横向速度变化。短周期的群速度分布同地表地质结构、地形密切相关；
The maps at short periods reveal an evident lateral heterogeneity in the crust of North-China, quite well in agreement with known geological and tectonic features.
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