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    • 5. 发明申请
    • METHOD OF AND APPARATUS FOR PROCESSING SEISMIC DATA
    • 用于处理地震数据的方法和装置
    • US20080275650A1
    • 2008-11-06
    • US12176356
    • 2008-07-19
    • Johan Olof Anders RobertssonAndrew CurtisDirk-Jan Van Manen
    • Johan Olof Anders RobertssonAndrew CurtisDirk-Jan Van Manen
    • G01V1/28
    • G01V1/286G01V1/362G01V2210/53
    • A method of processing seismic data that includes including first and second modes of seismic energy where the second mode has been generated by partial mode conversion of the first mode at a boundary face of a layer of the seabed includes the step of cross-correlating a trace acquired at a receiver and including events corresponding to the first mode with a trace acquired at the same receiver and including events corresponding to the second mode. An event in the cross-correlated data that corresponds to partial mode conversion is identified, and the amplitude of this event is normalized, for example relative to the amplitude of the peak in the cross-correlogram at zero time delay. Information about the effects of the static shift produced by the layer and/or about vector infidelity can be arrived from normalized cross-correlograms for receivers in a receiver array.
    • 一种处理地震数据的方法,包括包括地震能量的第一和第二模式,其中通过在海底层的边界面处的第一模式的部分模式转换已经产生第二模式,包括将迹线互相关的步骤 在接收机处获取并且包括与在第一模式相对应的事件,其中在同一接收机处获取的跟踪包括与第二模式对应的事件。 识别对应于部分模式转换的交叉相关数据中的事件,并且该事件的幅度例如相对于零时间延迟的交叉相关中的峰值的幅度被归一化。 关于由层产生的静态移位和/或关于向量不忠的影响的信息可以从接收机阵列中的接收机的标准化交叉相关图得出。
    • 8. 发明授权
    • Method of and apparatus for processing seismic data
    • 地震数据处理方法及装置
    • US07418349B2
    • 2008-08-26
    • US10502451
    • 2003-01-20
    • Johan Olof Anders RobertssonAndrew CurtisDirk-Jan Van Manen
    • Johan Olof Anders RobertssonAndrew CurtisDirk-Jan Van Manen
    • G01V1/00G01V1/38
    • G01V1/286G01V1/362G01V2210/53
    • A method of processing seismic data that includes including first and second modes of seismic energy where the second mode has been generated by partial mode conversion of the first mode at a boundary face of a layer of the seabed includes the step of cross-correlating a trace acquired at a receiver and including events corresponding to the first mode with a trace acquired at the same receiver and including events corresponding to the second mode. An event in the cross-correlated data that corresponds to partial mode conversion is identified, and the amplitude of this event is normalized, for example relative to the amplitude of the peak in the cross-correlogram at zero time delay. Information about the effects of the static shift produced by the layer and/or about vector infidelity can be arrived from normalized cross-correlograms for receivers in a receiver array.
    • 一种处理地震数据的方法,包括包括地震能量的第一和第二模式,其中通过在海底层的边界面处的第一模式的部分模式转换已经产生第二模式,包括将迹线互相关的步骤 在接收机处获取并且包括与在第一模式相对应的事件,其中在同一接收机处获取的跟踪包括与第二模式对应的事件。 识别对应于部分模式转换的交叉相关数据中的事件,并且该事件的幅度例如相对于零时间延迟的交叉相关中的峰值的幅度被归一化。 关于由层产生的静态移位和/或关于向量不忠的影响的信息可以从接收机阵列中的接收机的标准化交叉相关图得出。
    • 10. 发明授权
    • Method of and apparatus for processing seismic data
    • 地震数据处理方法及装置
    • US07715987B2
    • 2010-05-11
    • US12176356
    • 2008-07-19
    • Johan Olof Anders RobertssonAndrew CurtisDirk-Jan Van Manen
    • Johan Olof Anders RobertssonAndrew CurtisDirk-Jan Van Manen
    • G01V1/00G01V1/38
    • G01V1/286G01V1/362G01V2210/53
    • A method of processing seismic data that includes including first and second modes of seismic energy where the second mode has been generated by partial mode conversion of the first mode at a boundary face of a layer of the seabed includes the step of cross-correlating a trace acquired at a receiver and including events corresponding to the first mode with a trace acquired at the same receiver and including events corresponding to the second mode. An event in the cross-correlated data that corresponds to partial mode conversion is identified, and the amplitude of this event is normalized, for example relative to the amplitude of the peak in the cross-correlogram at zero time delay. Information about the effects of the static shift produced by the layer and/or about vector infidelity can be arrived from normalized cross-correlograms for receivers in a receiver array.
    • 一种处理地震数据的方法,包括包括地震能量的第一和第二模式,其中通过在海底层的边界面处的第一模式的部分模式转换已经产生第二模式,包括将迹线互相关的步骤 在接收机处获取并且包括与在第一模式相对应的事件,其中在同一接收机处获取的跟踪包括与第二模式对应的事件。 识别对应于部分模式转换的交叉相关数据中的事件,并且该事件的幅度例如相对于零时间延迟的交叉相关中的峰值的幅度被归一化。 关于由层产生的静态移位和/或关于向量不忠的影响的信息可以从接收机阵列中的接收机的标准化交叉相关图得出。