SEGMENTED BASE PLATE SEISMIC SWEEPS
    31.
    发明申请
    SEGMENTED BASE PLATE SEISMIC SWEEPS 有权
    SEGMENTED基板地震

    公开(公告)号:US20160170048A1

    公开(公告)日:2016-06-16

    申请号:US14964823

    申请日:2015-12-10

    CPC classification number: G01V1/005

    Abstract: Vibrators for producing seismic signals for use in oil and gas exploration are equipped with segmented base plates, each segment being independently controlled and activated. The use of an array of base plate segments allows the individual segments of the array to be activated in a particular pattern, thus generating S-waves and other unconventional wave patterns for seismic use.

    Abstract translation: 用于生产用于石油和天然气勘探的地震信号的振动器装备有分段基板,每个段被独立控制和激活。 使用基板段的阵列允许阵列的各个段以特定的模式被激活,从而产生用于地震的S波和其它非常规的波形图。

    MARINE DETERMINISTIC NOTCH COMPENSATION
    32.
    发明申请
    MARINE DETERMINISTIC NOTCH COMPENSATION 审中-公开
    海洋确定性补偿

    公开(公告)号:US20160047931A1

    公开(公告)日:2016-02-18

    申请号:US14817718

    申请日:2015-08-04

    Abstract: A method of performing notch compensation and a system to perform notch compensation for a first seismic streamer are described. The method includes disposing the first seismic streamer at a first depth, where the seismic streamer includes a first set of sensors to receive reflections resulting from a seismic source, the reflections indicating a notch at a frequency. The method also includes disposing a second seismic streamer at a second depth, the second depth being less than the first depth and the second seismic streamer including a second set of sensors to receive reflections resulting from the seismic source. The method further includes processing the reflections received by the first set of sensors and the second set of sensors together to derive the match filter, and applying the match filter to the reflections received by the first set of sensors of the first seismic streamer to compensate for the notch.

    Abstract translation: 描述了执行缺口补偿的方法和对第一地震拖缆执行陷波补偿的系统。 该方法包括将第一地震拖缆放置在第一深度处,其中地震拖缆包括第一组传感器以接收由地震源产生的反射,反射指示频率处的陷波。 该方法还包括在第二深度处布置第二地震拖缆,第二深度小于第一深度,第二地震拖缆包括第二组传感器以接收由地震源产生的反射。 该方法还包括将由第一组传感器和第二组传感器接收的反射处理在一起以导出匹配滤波器,以及将匹配滤波器应用于由第一地震拖缆的第一组传感器接收的反射,以补偿 缺口

    MAGNETIC FIELD MEASUREMENT VIA STREAMER CABLES
    33.
    发明申请
    MAGNETIC FIELD MEASUREMENT VIA STREAMER CABLES 审中-公开
    磁场测量通过流动电缆

    公开(公告)号:US20150355362A1

    公开(公告)日:2015-12-10

    申请号:US14709838

    申请日:2015-05-12

    Abstract: A method of generating a magnetic anomaly map and a system to develop a magnetic anomaly map are described. The method includes obtaining magnetic compass data recorded by two or more magnetic compasses disposed along a seismic streamer that traverses a first area and obtaining measurements from one or more navigation systems over the first area. The method also includes determining a correct position of each of the two or more magnetic compasses based on the measurements from the one or more navigation systems, and comparing the magnetic compass data with theoretical magnetic field data at the correct positions to generate a magnetic anomaly map.

    Abstract translation: 描述了产生磁异常图的方法和开发磁异常图的系统。 该方法包括获得由沿着穿过第一区域的地震拖缆设置的两个或更多个磁罗盘记录的磁罗盘数据,并从第一区域上的一个或多个导航系统获得测量值。 该方法还包括基于来自一个或多个导航系统的测量值确定两个或多个磁罗盘中的每一个的正确位置,以及将磁罗盘数据与正确位置处的理论磁场数据进行比较以产生磁异常图 。

    COMPRESSIVE SENSING
    34.
    发明申请
    COMPRESSIVE SENSING 有权
    压缩感应

    公开(公告)号:US20150124560A1

    公开(公告)日:2015-05-07

    申请号:US14529690

    申请日:2014-10-31

    Abstract: Computer-implemented method for determining optimal sampling grid during seismic data reconstruction includes: a) constructing an optimization model, via a computing processor, given by minu∥Su∥1 s.t. ∥Ru−b∥2≦σ wherein S is a discrete transform matrix, b is seismic data on an observed grid, u is seismic data on a reconstruction grid, and matrix R is a sampling operator; b) defining mutual coherence as μ ≤ C S  m ( log   n ) 6 , wherein C is a constant, S is a cardinality of Su, m is proportional to number of seismic traces on the observed grid, and n is proportional to number of seismic traces on the reconstruction grid; c) deriving a mutual coherence proxy, wherein the mutual coherence proxy is a proxy for mutual coherence when S is over-complete and wherein the mutual coherence proxy is exactly the mutual coherence when S is a Fourier transform; and d) determining a sample grid r*=arg minr μ(r).

    Abstract translation: 用于在地震数据重建期间确定最佳采样网格的计算机实现的方法包括:a)通过计算处理器构建优化模型,由minu|Su‖1s.t.t给出。 ∥Ru-b‖2≦̸&sgr; 其中S是离散变换矩阵,b是观测网格上的地震数据,u是重建网格上的地震数据,矩阵R是采样算子; b)将相互相干定义为μ≤CCSm(对数n)6,其中C是常数,S是Su的基数,m与观察到的网格上的地震轨迹数成比例,并且n与 重建网格上的地震轨迹数; c)导出相互一致性代理,其中当S超过完成时,相互连贯代理是相互一致性的代理,并且其中当S是傅立叶变换时,相互连贯代理恰好是相互相干; 和d)确定样本网格r * = arg minrμ(r)。

    CRITICAL REFLECTION ILLUMINATIONS ANALYSIS
    36.
    发明申请
    CRITICAL REFLECTION ILLUMINATIONS ANALYSIS 有权
    关键反射照明分析

    公开(公告)号:US20130155814A1

    公开(公告)日:2013-06-20

    申请号:US13718159

    申请日:2012-12-18

    CPC classification number: G01V1/345 G01V1/301 G01V1/303 G01V2200/14

    Abstract: The illumination/imaging of a theorized target horizon that is below a theorized velocity contrast horizon where the velocity contrast horizon may represent the bottom of a salt dome by assessing the path of seismic energy for critical angle reflection/refraction and tabulates the successful paths and unsuccessful paths. For some subsurface locations, seismic energy will not reach the surface above the velocity contrast due to the shapes of the velocity contrast horizon and target horizon and the velocity model through which the studied waves propagate. Displays may be prepared and used for understanding illumination/imaging of the geology for drilling, reacquisition, and reprocessing to elicit information about subsurface geology that may have been overlooked or ignored. Future surveys avoid expensive surveying which cannot obtain useful seismic data as determined by the velocity contrast for the target locations due to the shapes of the horizons and the velocity model.

    Abstract translation: 理论上的目标地平线的照明/成像低于理论速度对比度水平线,其中速度对比度边界可以通过评估临界角反射/折射的地震能量的路径来表示盐穹顶的底部,并列出成功的路径和不成功 路径。 对于一些地下位置,由于速度对比度水平和目标水平的形状以及研究的波传播的速度模型,地震能量将不会到达速度对比度以上的表面。 显示器可以准备并用于理解用于钻井,再采集和再处理的地质学的照明/成像,以引出可能被忽视或忽略的地下地质信息。 未来的调查避免了昂贵的测量,由于地平线和速度模型的形状,无法获得由目标位置的速度对比度确定的有用的地震数据。

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