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    • 2. 发明申请
    • SYSTEM AND METHOD FOR PROCESSING 4D SEISMIC DATA
    • 用于处理4D地震数据的系统和方法
    • US20130253838A1
    • 2013-09-26
    • US13804029
    • 2013-03-14
    • Sandra Tegtmeier-LastGilles Hennenfent
    • Sandra Tegtmeier-LastGilles Hennenfent
    • G01V1/36
    • G01V1/32G01V1/308G01V2210/48G01V2210/612G01V2210/6122
    • A system and method for determining a 4D difference from 4D seismic data including receiving a baseline seismic dataset and a monitor seismic dataset; identifying a 4D signal present in the monitor seismic dataset to create a 4D monitor dataset and a signal in the baseline seismic dataset which matches the monitor seismic dataset to create a baseline matching signal dataset; differencing the baseline matching signal dataset and the baseline seismic dataset to create a 4D baseline dataset; and differencing the 4D baseline dataset and the 4D monitor dataset to create a 4D difference dataset. In an embodiment, a multi-scale, multi-directional transform is used to identify the 4D signal present in the monitor seismic dataset and the signal in the baseline seismic dataset which matches the monitor seismic dataset.
    • 一种用于从4D地震数据确定4D差异的系统和方法,包括接收基线地震数据集和监测地震数据集; 识别存在于监测地震数据集中的4D信号,以创建与监测地震数据集匹配的基线地震数据集中的4D监测数据集和信号,以创建基线匹配信号数据集; 区分基线匹配信号数据集和基线地震数据集,以创建4D基线数据集; 并区分4D基准数据集和4D监测数据集,以创建4D差异数据集。 在一个实施例中,使用多尺度多方向变换来识别存在于监测地震数据集中的4D信号和与监测地震数据集匹配的基线地震数据集中的信号。
    • 3. 发明授权
    • Predicting interbed multiples in seismic data using beam decomposition
    • 使用光束分解预测地震数据中的间隔倍数
    • US09588244B2
    • 2017-03-07
    • US13951108
    • 2013-07-25
    • Tamas NemethSandra Tegtmeier-LastN. Ross HillYue WangPeeter AkerbergShoujian Huang
    • Tamas NemethSandra Tegtmeier-LastN. Ross HillYue WangPeeter AkerbergShoujian Huang
    • G01V1/00G01V9/00G01V1/30G01V1/36
    • G01V1/30G01V1/36G01V2210/56G01V2210/671
    • A method of attenuating interbed multiples in multiply-reflected seismic waves is performed at a computer system, the method including: providing multiple beams of seismic data and an earth model related to a geological volume; selecting one of the beams as an input beam associated with a pair of source and detector located near a top surface of the geological volume; determining at least one of (i) a source-side stationary pegleg arrival and a corresponding detector-side primary beam and (ii) a detector-side stationary pegleg arrival and a corresponding source-side primary beam; predicting an interbed multiples beam using at least one of (i) the detector-side primary beam delayed by the source-side stationary pegleg arrival and (ii) the source-side primary beam delayed by the detector-side stationary pegleg arrival; and deconvolving the predicted interbed multiples beam with the input beam to remove at least a portion of interbed multiples present in the input beam.
    • 在计算机系统中执行衰减多重反射地震波中的相互叠加倍数的方法,该方法包括:提供地震数据的多个波束和与地质体相关的地球模型; 选择一个光束作为与位于地质体积的顶表面附近的一对源和检测器相关联的输入光束; 确定(i)源极侧固定盖子到达和相应的检测器侧主波束中的至少一个以及(ii)检测器侧静止佩戴者到达和相应的源侧主波束; 使用以下中的至少一个预测中间多重波束:(i)由源极侧固定佩戴者到达延迟的检测器侧主波束和(ii)由检测器侧静止佩格尔到达延迟的源侧主波束; 并用输入光束去除预测的中间多重波束,以去除存在于输入光束中的至少一部分的中间多个波束。
    • 5. 发明申请
    • PREDICTING INTERBED MULTIPLES IN SEISMIC DATA USING BEAM DECOMPOSITION
    • 使用光束分解预测地震数据中的互动多项式
    • US20150032378A1
    • 2015-01-29
    • US13951108
    • 2013-07-25
    • Tamas NemethSandra Tegtmeier-LastN. Ross HillYue WangPeeter AkerbergShoujian Huang
    • Tamas NemethSandra Tegtmeier-LastN. Ross HillYue WangPeeter AkerbergShoujian Huang
    • G01V1/30
    • G01V1/30G01V1/36G01V2210/56G01V2210/671
    • A method of attenuating interbed multiples in multiply-reflected seismic waves is performed at a computer system, the method comprising: providing multiple beams of seismic data and an earth model related to a geological volume; selecting one of the beams as an input beam associated with a pair of source and detector located near a top surface of the geological volume; determining at least one of (i) a source-side stationary pegleg arrival and a corresponding detector-side primary beam and (ii) a detector-side stationary pegleg arrival and a corresponding source-side primary beam; predicting an interbed multiples beam using at least one of (i) the detector-side primary beam delayed by the source-side stationary pegleg arrival and (ii) the source-side primary beam delayed by the detector-side stationary pegleg arrival; and deconvolving the predicted interbed multiples beam with the input beam to remove at least a portion of interbed multiples present in the input beam.
    • 在计算机系统中执行衰减多重反射地震波中的层间倍数的方法,该方法包括:提供地震数据的多个波束和与地质体积相关的地球模型; 选择一个光束作为与位于地质体积的顶表面附近的一对源和检测器相关联的输入光束; 确定(i)源极侧固定盖子到达和相应的检测器侧主波束中的至少一个以及(ii)检测器侧静止佩戴者到达和相应的源侧主波束; 使用以下中的至少一个预测中间多重波束:(i)由源极侧固定佩戴者到达延迟的检测器侧主波束和(ii)由检测器侧静止佩格尔到达延迟的源侧主波束; 并用输入光束去除预测的中间多重波束,以去除存在于输入光束中的至少一部分的中间多个波束。