• 结果表明地壳上地幔结构纵向横向具有明显的不均匀性。

    The results show that the crust and upper mantle structures present obvious lateral and vertical inhomogeneity.

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  • 区域地震波携带着大量信息,可以很好地反映地壳地幔结构变化

    Regional seismic wave carries lots of information about structural variations in the crust and the upper mantle.

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  • 负荷潮汐改正地壳地幔结构密切关系,主要原因是负荷潮汐取决于高阶勒夫数。

    There is close relation between loading tidal correction and structure of crust and upper mantle.

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  • 述三类型地壳结构差异主要地幔物质地壳垂直迁移程度不同造成的。

    The difference between different crustal structures may be largely due to the difference in degree of vertical migration of-materials from the uppermost mantle into the crust.

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  • 本文研究利用天然地震PS转换波及PPP二次波到时资料反演地壳地幔速度结构尝试。

    An inversion of velocity structure of crust and upper mantle by using converted PS wave and multiwave PPP etc, is reported in this paper.

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  • 地壳上地幔S速度结构与强震关系和强震活动的深部背景进行探讨

    Study to the relation between strong earthquakes and S-wave velocity structures in the crust and upper mantle in the studied area.

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  • 本文详细研究了台湾澎湖列岛地幔幔源包体变形结构组构橄榄石位构造。

    This paper deals with deformation textures, petrofabrics and dislocation microstructures of olivine from the mantle-derived xenoliths in the Penghu Islands, Taiwan.

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  • 本区地幔变形事件结构特征表明福建东部和台湾澎湖列岛一带具有十分相似上地幔流变学特征。

    Deformation events and thermal textures of the upper mantle in this region show that Fujian and the Penghu Islands are characterized by a similar rheological state of the upper mantle.

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  • 文中提出了本区继续开展地壳地幔结构研究的任务设想

    The paper also proposes the tasks and tentative ideas to continuously conduct researches on crustal and upper mantal fine structures in this region.

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  • 揭示了剖面地壳地幔结构特征,进行了划分。

    The results show electric property structure of the crust and upper mantle clearly.

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  • 本文震源机制地震地质、地壳地幔速度结构资料为基础,研究青藏高原成因有关现代构造问题。

    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.

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  • 可以推断接收器功能S速度结构         五大连池火山区地壳地幔

    The S wave velocity structure is inferred from the receiver function for the crust and upper mantle of the Wudalianchi volcano area.

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  • 本文介绍应用闾阳—海城—东沟剖面深地震测深资料研究剖面地壳地幔密度结构结果

    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.

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  • 本文介绍应用闾阳—海城—东沟剖面深地震测深资料研究剖面地壳地幔密度结构结果

    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.

    youdao

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