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    • 3. 发明申请
    • Performing 3-D Scatterer Imaging From 2-D Seismic Data
    • 从二维地震数据进行三维散射体成像
    • US20080195321A1
    • 2008-08-14
    • US11674526
    • 2007-02-13
    • Stewart Arthur Levin
    • Stewart Arthur Levin
    • G01V1/34
    • G01V1/288
    • A method for analyzing seismic data from a formation. The method may first receive two-dimensional (2-D) seismic data of a formation comprising a number of individual seismic lines acquired over an exploration area and having a large interline spacing. The 2-D seismic data may then be preprocessed to enhance diffracted energy. For each respective hypothetical diffractor location, the method may then search for coherent diffraction arrivals on nearby 2-D seismic lines consistent with the respective hypothetical diffractor location. The method may then store information regarding identified diffractor locations. The method may then create a map based on the identified diffractor locations, wherein the map illustrates areas of high diffraction. The map may then be displayed on a display, wherein the map is useable to assess the formation.
    • 一种用于分析地层数据的方法。 该方法可以首先接收地层的二维(2-D)地震数据,该地层包括在勘探区域上获取并且具有大的间隔间隔的多个单独的地震线。 然后可以对2-D地震数据进行预处理以增强衍射能量。 对于每个各自的假想衍射器位置,该方法然后可以搜索与相应的假想衍射器位置一致的附近的2-D地震线上的相干衍射到达。 该方法然后可以存储关于识别的衍射器位置的信息。 该方法然后可以基于所识别的衍射器位置创建地图,其中该地图示出了高衍射的区域。 然后可以在显示器上显示地图,其中地图可用于评估地层。
    • 4. 发明申请
    • CROSSWELL SEISMIC SURVEYING IN A DEVIATED BOREHOLE
    • 隧道地震勘探在一个偏僻的洞穴
    • US20140257705A1
    • 2014-09-11
    • US14240782
    • 2011-09-09
    • Stewart Arthur Levin
    • Stewart Arthur Levin
    • G01V1/30E21B49/00
    • G01V1/30E21B49/00G01V1/42
    • First seismic data is collected from a plurality of points on a reflecting feature in the formation by emitting a first seismic signal from a first array of source locations in a deviated portion of a first borehole drilled through a formation and receiving first reflections of the first seismic signal from the reflecting feature by a first array of receiver locations in a deviated portion of a second borehole drilled through the formation. Second seismic data is collected from the plurality of points on the reflecting feature in the formation by emitting a second seismic signal from a second array of source locations in the deviated portion of the first borehole, the second array of source locations being different from the first array of source locations, and receiving second reflections of the second seismic signal from the plurality of points on the reflecting feature by a second array of receiver locations in the deviated portion of the second borehole. The collected first seismic data and the collected second seismic data are analyzed to draw conclusions about the formation. The conclusions about the formation are used to take an action concerning the formation.
    • 通过从穿过地层钻出的第一钻孔的偏离部分中的源位置的第一阵列发射第一地震信号并接收第一地震的第一反射,从地层中的反射特征上的多个点收集第一地震数据 来自反射特征的信号通过钻探穿过地层的第二钻孔的偏离部分中的接收器位置的第一阵列。 通过从第一钻孔的偏离部分的源位置的第二阵列发射第二地震信号,从地层中的反射特征上的多个点收集第二地震数据,源位置的第二阵列不同于第一地震信号 并且通过第二钻孔的偏离部分中的第二阵列的接收器位置从反射特征上的多个点接收第二地震信号的第二反射。 分析收集到的第一次地震资料和收集到的第二次地震资料,得出有关地层数据的结论。 关于形成的结论被用来采取有关形成的行动。
    • 5. 发明授权
    • Performing 3-D scatterer imaging from 2-D seismic data
    • 从二维地震数据进行三维散射体成像
    • US07545704B2
    • 2009-06-09
    • US11674526
    • 2007-02-13
    • Stewart Arthur Levin
    • Stewart Arthur Levin
    • G01V1/34G01V1/30
    • G01V1/288
    • A method for analyzing seismic data from a formation. The method may first receive two-dimensional (2-D) seismic data of a formation comprising a number of individual seismic lines acquired over an exploration area and having a large interline spacing. The 2-D seismic data may then be preprocessed to enhance diffracted energy. For each respective hypothetical diffractor location, the method may then search for coherent diffraction arrivals on nearby 2-D seismic lines consistent with the respective hypothetical diffractor location. The method may then store information regarding identified diffractor locations. The method may then create a map based on the identified diffractor locations, wherein the map illustrates areas of high diffraction. The map may then be displayed on a display, wherein the map is useable to assess the formation.
    • 一种用于分析地层数据的方法。 该方法可以首先接收地层的二维(2-D)地震数据,该地层包括在勘探区域上获取并且具有大的间隔间隔的多个单独的地震线。 然后可以对2-D地震数据进行预处理以增强衍射能量。 对于每个各自的假想衍射器位置,该方法然后可以搜索与相应的假想衍射器位置一致的附近的2-D地震线上的相干衍射到达。 该方法然后可以存储关于识别的衍射器位置的信息。 该方法然后可以基于所识别的衍射器位置创建地图,其中该地图示出了高衍射的区域。 然后可以在显示器上显示地图,其中地图可用于评估地层。