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    • 21. 发明申请
    • Methods for Controlling Marine Seismic Equipment Orientation During Acquisition of Marine Seismic Data
    • 海洋地震资料采集期间海洋抗震设备导向控制方法
    • US20080316859A1
    • 2008-12-25
    • US11767389
    • 2007-06-22
    • Kenneth E. WelkerJohan Olof Anders RobertssonJens Olav Paulsen
    • Kenneth E. WelkerJohan Olof Anders RobertssonJens Olav Paulsen
    • G01V1/38
    • G01V1/3826
    • Methods are described for actively steering a towed marine seismic component using one or more actively controllable control members; reducing the actively steering of the control members during duration of a time window of recording seismic reflections from a sub-surface geological feature of interest; and resuming the actively steering of the control members after the time window. The marine seismic component may be a streamer, a source, or both. Other methods allow measuring initial orientation of a streamer based on measuring static control surface angle of a control surface of an inline steerable bird. This abstract is provided to comply with the rules requiring an abstract, and allow a reader to ascertain the subject matter of the technical disclosure. It will not be used to interpret or limit the scope or meaning of the claims. 37 CFR 1.72(b).
    • 描述了用于使用一个或多个主动控制的控制构件主动地转向牵引的海洋地震部件的方法; 在从感兴趣的地下地质特征记录地震反射的时间窗口的持续时间期间减少控制构件的主动转向; 并在时间窗口之后恢复控制构件的主动转向。 海洋地震成分可以是流光,源或两者。 其他方法允许基于测量内联可操纵鸟的控制表面的静态控制表面角来测量拖缆的初始取向。 提供本摘要以符合要求摘要的规则,并允许读者确定技术公开的主题。 它不会用于解释或限制权利要求的范围或含义。 37 CFR 1.72(b)。
    • 22. 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。