METHODS AND SYSTEMS FOR SEISMIC MODELING USING MULTIPLE SEISMIC SOURCE TYPES
    1.
    发明申请
    METHODS AND SYSTEMS FOR SEISMIC MODELING USING MULTIPLE SEISMIC SOURCE TYPES 审中-公开
    使用多种地震源类型进行地震建模的方法与系统

    公开(公告)号:US20150346385A1

    公开(公告)日:2015-12-03

    申请号:US14649192

    申请日:2013-12-10

    Abstract: Seismic Modeling Using Multiple Seismic Sources. At least some of the illustrative embodiments are methods including: simulating an effect of multiple seismic sources concurrently on a geologic formation, the simulating by: reading data from a seismic source file, wherein the seismic source file describes at least two seismic source types; modeling, by a computer system, the concurrent propagation of acoustic energy from the at least two seismic sources types through the geologic formation; and generating a seismic output file.

    Abstract translation: 使用多个地震源的地震建模。 示例性实施例中的至少一些是包括:通过以下步骤模拟多个地震源的多个地震源的影响:模拟地震源文件中的数据,其中所述地震源文件描述至少两个地震源类型; 通过计算机系统建模,通过地质构造从至少两个地震源类型同时传播声能; 并产生地震输出文件。

    Structure tensor constrained tomographic velocity analysis

    公开(公告)号:US09869783B2

    公开(公告)日:2018-01-16

    申请号:US15025659

    申请日:2015-09-08

    CPC classification number: G01V1/303 G01V1/38

    Abstract: An example method for tomographic migration velocity analysis may include collecting seismographic traces from a subterranean formation and using an initial velocity model to generate common image gathers and a depth image volume based, at least in part, on the seismographic traces. A structure tensor may be computed with the depth image volume for automated structural dip and azimuth estimation. A semblance may be generated using said plurality of common image gathers and said structure tensor. Image depth residuals may be automatically picked from said semblance. A ray tracing computation may be performed on said initial velocity models using said structure tensor. An updated velocity model may be generated with a tomographic inversion computation, wherein said tomographic inversion computation uses said plurality of image depth residuals and said ray tracing computation.

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