• Reflections are the main carriers of subsurface structures, and also the main information used in seismic imaging.

    反射波是地下构造信息的主要载体,是地震成像的主要信息。

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  • Compressive tectonic stress is the main stress in foreland basins in western China, where surface and subsurface structures are very complicated.

    中国西部前陆盆地主要以挤压构造应力为主,地表与地下构造异常复杂。

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  • Distinct seismic reflection configuration reveals the subsurface structures, which provides a solid base of accurate seismic data interpretation.

    清晰的地震反射结构突出了特定的地质现象,为地震资料的准确标定提供了依据。

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  • Stratigraphic division is challenging in the eastern Sichuan Basin due to the large amplitude of structural high, highly developed faults and complex subsurface structures.

    四川盆地川东地区地质构造隆起幅度高,断层发育,地下构造复杂,地层分层困难。

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  • As a direct and accurate inversion method of subsurface structures, VSP processing is one of the most important approaches to identify complex subtle oil and gas reservoirs.

    VSP处理方法反演地下结构直接、精确,是寻找复杂构造的、隐蔽的油气藏的最重要的方法系列之一。

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  • Laminated imaging of the subsurface structures of materials has been successfully realized by this technique because thermal waves are heavily damped and have short wavelengths.

    由于热波是一种高衰减波,且波长短,现已成功地实现了对材料亚表面结构的分层成像。

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  • The subsurface structures of the Kuqa rejuvenated foreland basin are really complex, so a correct interpretation of them is the key for understanding the genesis of the basin and hydrocarbon traps.

    库车再生前陆盆地地下构造复杂,正确的构造解释就成为了解盆地成因机理和油气圈闭的关键所在。

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  • Seismic migration technique has become an important means for analysing all complicated subsurface geological structures.

    地震偏移技术已经成为研究一切复杂地下介质结构的主要手段。

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  • The delay or difference in the arrival time of seismic events that can result from weathering of the rocks or variations in geologic structures in the subsurface.

    地震同相轴到达时的延迟或差异,这是由于岩石的风化层和地下地质体的变化产生的。

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  • The delay or difference in the arrival time of seismic events that can result from weathering of the rocks or variations in geologic structures in the subsurface.

    地震同相轴到达时的延迟或差异,这是由于岩石的风化层和地下地质体的变化产生的。

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