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    • 1. 发明申请
    • Methods for acquiring and processing seismic data from quasi-simultaneously activated translating energy sources
    • 从准同步激活的翻译能源获取和处理地震数据的方法
    • US20050128874A1
    • 2005-06-16
    • US10736951
    • 2003-12-15
    • E. HerkenhoffJoseph Stefani
    • E. HerkenhoffJoseph Stefani
    • G01V1/00G01V1/02G01V1/38
    • G01V1/005G01V1/003G01V1/36G01V1/3808G01V2210/32
    • A method for obtaining seismic data is disclosed. A constellation of seismic energy sources is translated along a survey path. The seismic energy sources include a reference energy source and a satellite energy source. The reference energy source is activated and the satellite energy source is activated at a time delay relative to the activation of the reference energy source. This is repeated at each of the spaced apart activation locations along the survey path to generate a series of superposed wavefields. The time delay is varied between each of the spaced apart activation locations. Seismic data processing comprises sorting the traces into a common-geometry domain and replicating the traces into multiple datasets associated with each particular energy source. Each trace is time adjusted in each replicated dataset in the common-geometry domain using the time delays associated with each particular source. This result in signals generated from that particular energy source being generally coherent while rendering signals from the other energy source is generally incoherent. The coherent and incoherent signals are then filtered to attenuate incoherent signals.
    • 公开了一种获取地震数据的方法。 沿着勘测路径转换地震能源的一个星座。 地震能源包括参考能源和卫星能源。 参考能源被激活,并且卫星能量源以相对于参考能量源的激活的时间延迟被激活。 这在沿着测量路径的每个间隔开的激活位置处重复,以产生一系列叠加的波场。 时间延迟在每个间隔开的激活位置之间变化。 地震数据处理包括将迹线分类为公共几何域并将迹线复制到与每个特定能量源相关联的多个数据集中。 使用与每个特定源相关联的时间延迟,在公共几何域中的每个复制数据集中对每个跟踪进行时间调整。 这导致从该特定能源产生的信号通常是相干的,而来自另一能量源的信号通常是不相干的。 然后将相干和非相干信号滤波以衰减非相干信号。
    • 2. 发明申请
    • Methods for acquiring and processing seismic data from quasi-simultaneously activated translating energy sources
    • 从准同步激活的翻译能源获取和处理地震数据的方法
    • US20070272473A1
    • 2007-11-29
    • US10582682
    • 2004-12-06
    • E. HerkenhoffJoseph Stefani
    • E. HerkenhoffJoseph Stefani
    • G01V1/00
    • G01V1/005G01V1/003G01V1/36G01V1/3808G01V2210/32
    • A method for obtaining seismic data is disclosed. A constellation of seismic energy sources is translated along a survey path. The seismic energy sources include a reference energy source and a satellite energy source. The reference energy source is activated and the satellite energy source is activated at a time delay relative to the activation of the reference energy source. This is repeated at each of the spaced apart activation locations along the survey path to generate a series of superposed wavefields. The time delay is varied between each of the spaced apart activation locations. Seismic data processing comprises sorting the traces into a common-geometry domain and replicating the traces into multiple datasets associated with each particular energy source. Each trace is time adjusted in each replicated dataset in the common-geometry domain using the time delays associated with each particular source. This result in signals generated from that particular energy source being generally coherent while rendering signals from the other energy source is generally incoherent. The coherent and incoherent signals are then filtered to attenuate incoherent signals.
    • 公开了一种获取地震数据的方法。 沿着勘测路径转换地震能源的一个星座。 地震能源包括参考能源和卫星能源。 参考能源被激活,并且卫星能量源以相对于参考能量源的激活的时间延迟被激活。 这在沿着测量路径的每个间隔开的激活位置处重复,以产生一系列叠加的波场。 时间延迟在每个间隔开的激活位置之间变化。 地震数据处理包括将迹线分类为公共几何域并将迹线复制到与每个特定能量源相关联的多个数据集中。 使用与每个特定源相关联的时间延迟,在公共几何域中的每个复制数据集中对每个跟踪进行时间调整。 这导致从该特定能源产生的信号通常是相干的,而来自另一能量源的信号通常是不相干的。 然后将相干和非相干信号滤波以衰减非相干信号。
    • 3. 发明申请
    • Method and apparatus for true relative amplitude correction of seismic data for normal moveout stretch effects
    • 用于正常移动伸展效应的地震数据的真实相对幅度校正的方法和装置
    • US20060193205A1
    • 2006-08-31
    • US11056640
    • 2005-02-12
    • E. HerkenhoffRichard AlfordHarry Martin
    • E. HerkenhoffRichard AlfordHarry Martin
    • G01V1/28
    • G01V1/362G01V2210/52G01V2210/522
    • The present invention provides a method and apparatus for arriving at true relative amplitude destretched seismic traces from stretched seismic traces. The method compensates for offset varying reflection interference effects due to normal moveout. Stretch factors β and also input spectra are determined for NMOR stretched seismic traces. Estimates are then made of stretched wavelet spectra from the input spectra. A destretched wavelet spectra is then obtained. Shaping correction factors are determined by taking the ratio of the destretched wavelet spectra to the stretched wavelet spectra and are applied to the input spectra of the stretched traces to arrive at a destretched trace spectra. True relative amplitude scaling factors are computed by taking the ratio of a true relative amplitude property of the destretched wavelet spectra to a corresponding true relative amplitude property of the stretched wavelet spectra. Finally, the true relative amplitude scaling factors are applied to the destretched trace spectra to arrive at true relative amplitude destretched seismic traces.
    • 本发明提供一种用于从拉伸地震迹线到达真实的相对振幅破坏的地震迹线的方法和装置。 该方法补偿由于正常移动引起的偏移变化反射干扰效应。 确定NMOR拉伸地震迹线的拉伸因子β和输入光谱。 然后从输入光谱中估计拉伸的小波谱。 然后获得破坏的小波谱。 整形校正因子是通过将破坏后的小波谱与拉伸的小波光谱的比值进行确定的,并且应用于拉伸轨迹的输入光谱以得到一个残留的迹线光谱。 通过将破坏后的小波谱的真实相对振幅特性的比值与拉伸的小波频谱的对应的真实的相对振幅特性的比值来计算真实的相对幅度缩放因子。 最后,将真实的相对幅度缩放因子应用于残余的轨迹光谱,以得到真实的相对幅度破坏的地震迹线。