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    • 1. 发明申请
    • Method of and apparatus for processing seismic data
    • 地震数据处理方法及装置
    • US20060092764A1
    • 2006-05-04
    • US10502451
    • 2003-01-20
    • Johan RobertssonAndrew CurtisDirk-Jan Manen
    • Johan RobertssonAndrew CurtisDirk-Jan Manen
    • G01V1/00
    • 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 normalised, 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 normalised 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。
    • 2. 发明申请
    • CONSTRUCTION AND REMOVAL OF SCATTERED GROUND ROLL USING INTERFEROMETRIC METHODS
    • 使用干涉方法构造和去除散射地基滚子
    • US20070104028A1
    • 2007-05-10
    • US11458868
    • 2006-09-27
    • Dirk-Jan Van ManenJohan RobertssonAndrew Curtis
    • Dirk-Jan Van ManenJohan RobertssonAndrew Curtis
    • G01V1/00
    • G01V1/36G01V1/003G01V1/3808G01V3/12G01V2210/32
    • A data set can be corrected for the effects of interface waves by interferometrically measuring an interface wavefield between each of a plurality of planned locations within a survey area; and correcting survey data acquired in the survey area for the interface waves. The interface wavefield may be interferometrically measured by receiving a wavefield including interface waves propagating within a survey area, the survey area including a plurality of planned survey locations therein; generating interface wave data representative of the received interface wavefield; and constructing a Green's function between each of the planned survey positions from the interface wave data. Other aspects include an apparatus by which the interface wavefield may be interferometrically measured and a computer apparatus programmed to correct the seismic data using the interferometrically measured interface wave data.
    • 可以通过对测量区域内的多个计划位置中的每一个之间的界面波场进行干涉测量来校正接口波的影响的数据集; 并对接口波在调查区域获得的调查数据进行修正。 接口波场可以通过接收包括在测量区域内传播的界面波的波场来进行干涉测量,该测量区域包括多个计划的测量位置; 产生代表接收到的接口波场的接口波数据; 并从接口波数据构建每个计划的测量位置之间的格林函数。 其他方面包括可以对接口波场进行干涉测量的装置以及使用干涉测量的接口波数据编程来校正地震数据的计算机装置。
    • 4. 发明授权
    • Multi-component seismic data processing
    • 多分量地震数据处理
    • US07894298B2
    • 2011-02-22
    • US10568057
    • 2004-08-16
    • Dirk-Jan Van ManenAndrew CurtisJohan Robertsson
    • Dirk-Jan Van ManenAndrew CurtisJohan Robertsson
    • G01V1/00
    • G01V1/28G01V2210/20
    • There is described a method of moveout or velocity analysis of seismic signals using the steps of obtaining such signals 5 from a plurality of receivers, identifying receiver functions within the acoustic signals, analyzing said receiver functions for velocity or moveout characteristics, using the result of said analyzing step to determine, properties of multiple layers of earth located below said 10 receivers. The analyses can involve the use of representation of the traveltime differences as approximated power series of slowness or horizontal distances. The method is the first to comprehensively deal with a multi-layered earth or velocity model.
    • 描述了使用以下步骤从多个接收机获得这样的信号5的步骤,以识别声信号内的接收机功能,使用所述的信号的结果来分析所述接收机功能的速度或移动特性的步骤来进行地震信号的移动或速度分析的方法 分析步骤来确定位于所述10个接收器下面的多层地球的属性。 分析可以涉及将旅行时差的表示用作慢度或水平距离的近似幂级数。 该方法是首先全面处理多层地球或速度模型。
    • 7. 发明授权
    • Method of processing marine seismic data and a method of seismic surveying
    • 海洋地震资料处理方法及地震勘测方法
    • US07164619B2
    • 2007-01-16
    • US10466980
    • 2002-01-24
    • Johan RobertssonAndrew CurtisDirk-Jan Van Manen
    • Johan RobertssonAndrew CurtisDirk-Jan Van Manen
    • G01V1/36G01V1/38
    • G01V1/286
    • A method of determining seismic properties of a layer of the seabed, in particular a surface or near-surface layer (5), comprises directing seismic energy propagating in a first mode at a boundary face of the layer so as to cause partial mode conversion of the seismic energy at the boundary face. For example partial mode conversion may occur when seismic energy propagates upwards through the interface between a surface or near-surface layer (5) and the basement (6), owing to the difference in seismic properties between the surface or near-surface layer (5) and the basement (6). In the invention, the two modes of seismic energy—that is the initial mode and the mode generated by mode conversions at the interface—are received at a receiver. The difference in travel time of the two modes between the interface and the receiver is determined from the seismic data acquired by the receiver.
    • 确定海床,特别是表面或近表面层(5)的层的地震性质的方法包括指导在层的边界面处以第一模式传播的地震能量,以便导致部分模式转换 边界地震能量。 例如,由于表面或近表面层(5)之间的地震性质的差异,地震能量向上传播通过表面或近表面层(5)和基底(6)之间的界面,可能会发生部分模式转换 )和地下室(6)。 在本发明中,在接收机处接收地震能量的两种模式,即初始模式和由界面处的模式转换产生的模式。 根据接收机获取的地震数据,确定接口与接收机之间的两种模式的行进时间差。
    • 10. 再颁专利
    • Method and system for reducing effects of sea surface ghost contamination in seismic data
    • 减少地震数据中海面鬼影的影响的方法和系统
    • USRE41656E1
    • 2010-09-07
    • US11501195
    • 2000-03-21
    • Johan RobertssonJulian Edward KraghJames Edward Martin
    • Johan RobertssonJulian Edward KraghJames Edward Martin
    • G01V1/00G01V1/38
    • G01V1/3808G01V1/364G01V2210/56
    • An improved de-ghosting method and system that utilizes multi-component marine seismic data recorded in a fluid medium. The method makes use of two types of data: pressure data that represents the pressure in the fluid medium, such as sea water, at a number of locations; and vertical particle motion data that represents the vertical particle motion of the acoustic energy propagating in the fluid medium at a number of locations within the same spatial area as the pressure data. The vertical particle motion data can be in various forms, for example, velocity, pressure gradient, displacement, or acceleration. A spatial filter is designed so as to be effective at separating up and down propagating acoustic energy over substantially the entire range of non-horizontal incidence angles in the fluid medium. The spatial filter is applied to either the vertical particle motion data or to the pressure data, and then combined with the other data to generate pressure data that has its up and down propagating components separated.
    • 一种利用记录在流体介质中的多组分海洋地震数据的改进的去重影方法和系统。 该方法利用两种类型的数据:表示流体介质中的压力的​​压力数据,例如海水,在多个位置; 以及垂直粒子运动数据,其表示在与压力数据相同的空间区域内的多个位置处在流体介质中传播的声能的垂直粒子运动。 垂直粒子运动数据可以是各种形式,例如速度,压力梯度,位移或加速度。 空间滤波器被设计成在流体介质中基本上在非水平入射角的整个范围上分离上下传播的声能是有效的。 将空间滤波器应用于垂直粒子运动数据或压力数据,然后与其他数据组合以产生分离其上下传播分量的压力数据。