地震各向异性,地震学术语,已经发展成为在国际地震学和勘探地震学界具有重要影响的专题学术会议,曾受到联合国教科文组织(UNESCO),多个国际权威学术组织(AGU, EAGE, IASPEI, SEG等)和全球多家著名石油公司(Chevron, Shell, BP, ExxonMobil, Amoco等)的资助。
地震速度各向异性 seismic velocity anisotropy
It is significant to understand the characteristics of seismic anisotropy. In this thesis, the seismic anisotropy are comprehensively discussed, from the anisotropy research of origin to its theory and method.
本论文综述了地震各向异性研究的发展概况、起源,以及地震波在各向异性介质中传播的理论、方法。
参考来源 - 云南地区上地幔各向异性研究·2,447,543篇论文数据,部分数据来源于NoteExpress
快剪切波偏振方向与慢剪切波时间延迟是描述地震各向异性的两个主要参数。
The main parameters of shear-wave splitting are respectively polarization of fast shear-wave, and time delay of slow shear-wave.
地震波速度结构层析成像和地震各向异性分析,是推测现今地幔流动的主要观测依据。
The current inference of mantle flow is largely based on seismic tomography and anisotropic analysis.
地震各向异性研究不仅有助于准确认识地球内部精细结构,还有助于研究地球内部活动过程。
It is helpful to understand precisely the fine structure and the inner dynamic process of the globe to research it.
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