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    • 3. 发明申请
    • Interferometric Seismic Data Processing for a Towed Marine Survey
    • 牵引海洋调查的干涉地震数据处理
    • US20120081999A1
    • 2012-04-05
    • US12896643
    • 2010-10-01
    • David Fraser HallidayJulian Edward Kragh
    • David Fraser HallidayJulian Edward Kragh
    • G01V1/38G01V1/36
    • G01V1/28G01V1/364G01V1/38G01V2210/21G01V2210/32G01V2210/675
    • A method for processing seismic data. The method includes receiving the seismic data acquired at two or more sensors on a towed marine survey and regularizing the received seismic data into a spatial domain. After regularizing the seismic data, the method includes classifying the regularized seismic data below and equal to a predetermined frequency as low-frequency seismic data. The method then calculates a set of low-frequency Green's functions using interferometry on the low-frequency seismic data described above. The method then processes high-frequency seismic data of the seismic data to create a set of high-frequency Green's functions at one or more source locations of the towed marine survey. After creating the set of high-frequency Green's functions, the method merges the set of low-frequency Green's functions and the set of high-frequency Green's functions to create a set of broad-band Green's functions at the source locations.
    • 一种地震数据处理方法。 该方法包括接收在拖曳的海洋勘测中的两个或更多个传感器处获得的地震数据,并将接收的地震数据规范化为空间域。 在对地震数据进行正规化之后,该方法包括将低于和等于预定频率的正则化地震数据分类为低频地震数据。 该方法然后使用干涉测量对上述低频地震数据计算一组低频格林函数。 然后,该方法处理地震数据的高频地震数据,以在被拖曳的海洋勘测的一个或多个源位置创建一组高频格林函数。 在创建了一组高频绿色功能后,该方法融合了低频绿色功能和高频绿色功能的集合,以在源位置创建一组宽带绿色功能。
    • 4. 发明授权
    • Interferometric seismic data processing for a towed marine survey
    • 拖船测量的干涉地震数据处理
    • US08737165B2
    • 2014-05-27
    • US12896643
    • 2010-10-01
    • David Fraser HallidayJulian Edward Kragh
    • David Fraser HallidayJulian Edward Kragh
    • G01V1/28G01V1/38
    • G01V1/28G01V1/364G01V1/38G01V2210/21G01V2210/32G01V2210/675
    • A method for processing seismic data. The method includes receiving the seismic data acquired at two or more sensors on a towed marine survey and regularizing the received seismic data into a spatial domain. After regularizing the seismic data, the method includes classifying the regularized seismic data below and equal to a predetermined frequency as low-frequency seismic data. The method then calculates a set of low-frequency Green's functions using interferometry on the low-frequency seismic data described above. The method then processes high-frequency seismic data of the seismic data to create a set of high-frequency Green's functions at one or more source locations of the towed marine survey. After creating the set of high-frequency Green's functions, the method merges the set of low-frequency Green's functions and the set of high-frequency Green's functions to create a set of broad-band Green's functions at the source locations.
    • 一种地震数据处理方法。 该方法包括接收在拖曳的海洋勘测中的两个或更多个传感器处获得的地震数据,并将接收的地震数据规范化为空间域。 在对地震数据进行正规化之后,该方法包括将低于和等于预定频率的正则化地震数据分类为低频地震数据。 该方法然后使用干涉测量对上述低频地震数据计算一组低频格林函数。 然后,该方法处理地震数据的高频地震数据,以在被拖曳的海洋勘测的一个或多个源位置创建一组高频格林函数。 在创建一组高频绿色功能后,该方法合并了一组低频绿色功能和一组高频绿色功能,以在源位置创建一组宽带绿色功能。
    • 7. 发明授权
    • Processing seismic data
    • 处理地震数据
    • US07774142B2
    • 2010-08-10
    • US12098867
    • 2008-04-07
    • Lasse AmundsenTage RostenJohan O. A. RobertssonJulian Edward Kragh
    • Lasse AmundsenTage RostenJohan O. A. RobertssonJulian Edward Kragh
    • G01V1/00G01V1/38
    • G01V1/38G01V1/364G01V2210/56
    • A method of determining a vertical component of particle velocity from seismic data acquired using at least one receiver disposed within a water column includes determining the vertical component of particle velocity from the pressure at a first location and a second location. The first location is the location of a first receiver, and is vertically beneath the second location. The method uses an operator accurate for seismic data acquired at a vertical separation between the first and second locations of up to at least 0.4 times the minimum wavelength of seismic energy used to acquire the seismic data. The second location may be at or above the surface of the water column. Alternatively, the method may be applied to a twin streamer seismic surveying arrangement in which the second location is below the surface of the water column and is the location of a second receiver.
    • 使用设置在水柱内的至少一个接收器获取的地震数据确定粒子速度的垂直分量的方法包括从第一位置和第二位置处的压力确定粒子速度的垂直分量。 第一个位置是第一个接收器的位置,并且位于第二个位置之下。 该方法使用对于在用于获取地震数据的地震能量的最小波长的至少0.4倍的第一和第二位置之间的垂直间隔处获取的地震数据精确的操作者。 第二位置可以在水柱的表面上或上方。 或者,该方法可以应用于双拖缆地震测量装置,其中第二位置在水柱的表面下方并且是第二接收器的位置。