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    • 6. 发明申请
    • TRUE-AMPLITUDE LAYER-STRIPPING IN FRACTURED MEDIA
    • 破碎介质中的真振幅分层
    • WO2012154295A1
    • 2012-11-15
    • PCT/US2012/028545
    • 2012-03-09
    • EXXONMOBIL UPSTREAM RESEARCH COMPANYBANSAL, ReeshidevMATHENEY, Michael, P.LIU, Enru
    • BANSAL, ReeshidevMATHENEY, Michael, P.LIU, Enru
    • G01V1/00
    • G01V1/30G01V1/284
    • Method for determining fracture orientation and fracture intensity in multiple fractured layers in the subsurface in a layer-stripping manner. Multi-component, multi- azimuth seismic data are required (31), from which the horizontal, primarily converted wave, components are selected, and these data are further reduced by selecting only the data for which the survey azimuths are either parallel or perpendicular to the general fracture strike (33). If the general fracture trend is unknown, such selective data may be determined by an azimuth-offset scanning process. Layer stripping is performed on azimuth/offset stacks (42) to produce fracture parameter maps (43). All offsets are stacked in those azimuths that produce consistent fracture parameter maps (44), then layer stripping is performed (45) on the stacks to produce final fracture orientation and S-wave time difference maps (46). These maps can be used to produce true amplitude fast and slow S-waves (56).
    • 以层剥离方式确定地下多层断层的断裂取向和断裂强度的方法。 需要多分量,多方位地震数据(31),从中选择水平,主要转换波的分量,并通过仅选择测量方位平行或垂直的数据进一步减少这些数据 一般断裂(33)。 如果总体断裂趋势是未知的,则这种选择性数据可以通过方位偏移扫描过程来确定。 在方位角/偏移叠层(42)上执行层剥离以产生断裂参数图(43)。 所有偏移量都堆积在产生一致断裂参数图(44)的那些方位角上,然后在堆叠上进行层剥离(45)以产生最终断裂取向和S波时间差图(46)。 这些地图可用于产生真正的振幅快速和慢速S波(56)。
    • 10. 发明公开
    • TRUE-AMPLITUDE LAYER-STRIPPING IN FRACTURED MEDIA
    • 弗吉尼亚州中医药学院麻省理工学院
    • EP2707756A1
    • 2014-03-19
    • EP12781637.9
    • 2012-03-09
    • Exxonmobil Upstream Research Company
    • BANSAL, ReeshidevMATHENEY, Michael, P.LIU, Enru
    • G01V1/00
    • G01V1/30G01V1/284
    • Method for determining fracture orientation and fracture intensity in multiple fractured layers in the subsurface in a layer-stripping manner. Multi-component, multi-azimuth seismic data are required (31), from which the horizontal, primarily converted wave, components are selected, and these data are further reduced by selecting only the data for which the survey azimuths are either parallel or perpendicular to the general fracture strike (33). If the general fracture trend is unknown, such selective data may be determined by an azimuth-offset scanning process. Layer stripping is performed on azimuth/offset stacks (42) to produce fracture parameter maps (43). All offsets are stacked in those azimuths that produce consistent fracture parameter maps (44), then layer stripping is performed (45) on the stacks to produce final fracture orientation and S-wave time difference maps (46). These maps can be used to produce true amplitude fast and slow S-waves (56).
    • 以层剥离方式确定地下多层断层的断裂取向和断裂强度的方法。 需要多分量,多方位地震数据(31),从中选择水平,主要转换的波分量,并通过仅选择测量方位平行或垂直的数据进一步减少这些数据 一般断裂(33)。 如果总体断裂趋势是未知的,则这种选择性数据可以通过方位偏移扫描过程来确定。 在方位/偏移叠层(42)上执行层剥离以产生断裂参数图(43)。 所有偏移量都堆积在产生一致的断裂参数图(44)的那些方位角上,然后在堆叠上执行层剥离(45)以产生最终断裂取向和S波时间差图(46)。 这些地图可用于产生真正的振幅快速和慢速S波(56)。