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    • 4. 发明申请
    • Method for determining seafloor roughness using multibeam echosounder
    • 使用多波束回波测定海底粗糙度的方法
    • US20020173916A1
    • 2002-11-21
    • US09814104
    • 2001-03-22
    • Bishwajit ChakrabortyVijay N. Kodagali
    • G01V001/28
    • G01V1/28G01V1/38G01V2210/58
    • The present invention provides a method for determining sea floor roughness using multibeam echosounder, said method comprising providing backscatter, bathymetry and multibeam operational parameters; removing system gain from the backscatter data to obtain real seafloor backscatter data; calculating across track seafloor slope; incorporating correction factor in actual beam arrival angles; calculating seafloor area; measuring backscatter strength; obtaining backscatter strength data at 1null angle; obtaining power law parameters; using the above-obtained parameters in a seafloor roughness power law model; splicing the multibeam backscatter data; including sediment volume roughness model; and verifying the validity of the composite roughness model.
    • 本发明提供一种使用多波束回波测定确定海底粗糙度的方法,所述方法包括提供反向散射,测深和多波束操作参数; 从后向散射数据中去除系统增益,以获得真实的海底反向散射数据; 计算跨轨海底坡度; 将校正因子并入实际光束到达角度; 计算海底面积; 测量反向散射强度; 获得1°角的后向散射强度数据; 获得幂律参数; 在海底粗糙度幂律模型中使用上述参数; 拼接多波束反向散射数据; 包括沉积物体积粗糙度模型; 并验证复合粗糙度模型的有效性。
    • 8. 发明授权
    • Seismic true estimated wavelet
    • 地震真实估计小波
    • US08958267B2
    • 2015-02-17
    • US13469857
    • 2012-05-11
    • Peter M. EickJoel D. Brewer
    • Peter M. EickJoel D. Brewer
    • G01V1/00
    • G01V1/37G01V2210/127G01V2210/58
    • The invention relates to processing seismic data that includes signals from at least two sources and typically three or four sources where source separation is necessary for geophysical analysis. Specifically, the present invention is a process for correcting data prior to inversion where the correction is provided to correct for the filtering effect of the earth. The earth is a non-homogenous seismic propagator that causes distortions of wavelets of seismic energy related to the source and receiver azimuth and offset that makes the identification of source specific data within the composite data harder to identify. Computing an earth response and correcting for the effects of the earth on the wavelets provides for more resolution and more clarity in the resulting data and better geophysical interpretation.
    • 本发明涉及处理地震数据,其包括来自至少两个源的信号,通常三个或四个源,其中源分离对于地球物理分析是必需的。 具体地说,本发明是一种用于在反转之前对数据进行校正的处理,其中提供校正以校正地球的滤波效果。 地球是一种不均匀的地震传播器,其导致与源和接收机方位角和偏移量相关的地震能量小波的变形,这使得复合数据内的源特定数据的识别难以识别。 计算地球反应并纠正地球对小波的影响提供了更多的分辨率和更清晰的结果数据和更好的地球物理解释。
    • 10. 发明授权
    • Seismogram correction for absorption effects
    • 地震记录校正吸收效果
    • US07574303B2
    • 2009-08-11
    • US11760629
    • 2007-06-08
    • Ralf Ferber
    • Ralf Ferber
    • G01V1/28G06F19/00
    • G01V1/364G01V2210/58
    • Correcting seismograms to compensate for absorption or dissipative effects that occur in the earth. In one implementation, a ratio of traveltime (t) to absorption parameter (Q) may be computed for each seismogram. The ratio may be referred to as R. Further, the ratio may be computed for a predetermined set of traveltimes. As a result, a system of linear equations may be generated, where each ratio is represented by a linear equation having a number of unknown components. The system of linear equations may then be solved for the unknown components. The solved components may then be recombined or added to generate an estimate of R. In one implementation, only a portion of the solved components may be added. The seismograms may then be corrected using the estimate of R. As such, the seismograms may be corrected for absorption effects in a surface consistent manner.
    • 校正地震图以补偿地球中发生的吸收或耗散效应。 在一个实施方案中,可以针对每个地震图计算旅行时间(t)与吸收参数(Q)的比率。 该比率可以被称为R.此外,可以针对预定的行程组计算该比率。 结果,可以产生线性方程组,其中每个比率由具有多个未知分量的线性方程表示。 然后可以为未知组件求解线性方程组。 然后可以将所解决的组件重新组合或添加以产生R的估计。在一个实现中,可以仅添加一部分被求解的组件。 然后可以使用R的估计来校正地震图。因此,可以以表面一致的方式校正地震图的吸收效应。