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    • 1. 发明申请
    • Method for three dimensional seismic travel time tomography in transversely isotropic media
    • 横向各向同性介质三维地震行程时间层析成像方法
    • US20090213692A1
    • 2009-08-27
    • US12070966
    • 2008-02-22
    • Ruben D. MartinezJunru Jiao
    • Ruben D. MartinezJunru Jiao
    • G01V1/28
    • G01V1/303G01V1/28G01V2210/626G01V2210/66
    • A method for estimating seismic velocities in vertically transversely isotropic media includes generating an initial estimate of vertical interval velocity and interval normal moveout velocity with respect to depth from seismic data. An initial estimate is generated of a first anisotropy parameter with respect to depth. The first anisotropy parameter is related to the interval normal moveout velocity and the interval vertical velocity. An initial estimate is generated with respect to depth of a second anisotropy parameter. The second anisotropy parameter is related to the first anisotropy parameter and an interval anelliptic parameter. A first tomographic inversion is performed with respect to the interval normal moveout velocity and the second anisotropy parameter at a constant value of the first anisotropy parameter until travel time differentials reach minimum values. Layer depths are adjusted with the initial estimate of vertical interval velocity. Using values of the second anisotropy parameter determined in the first tomographic inversion, a second tomographic inversion is performed of interval normal moveout velocity and the first anisotropy parameter with respect to depth. The adjusted layer depths, interval normal moveout velocities and interval vertical velocities are again adjusted and interval anelliptic parameters are calculated from the second tomographic inversion.
    • 用于估计垂直横向各向同性介质中的地震速度的方法包括相对于地震数据的深度产生垂直间隔速度和间隔正常移动速度的初始估计。 产生关于深度的第一各向异性参数的初始估计。 第一个各向异性参数与间隔正常移动速度和间隔垂直速度有关。 相对于第二各向异性参数的深度产生初始估计。 第二个各向异性参数与第一各向异性参数和间隔椭圆参数有关。 在第一各向异性参数的恒定值下,相对于间隔正常移动速度和第二各向异性参数执行第一层析反转,直到行进时间差达到最小值。 层深度用垂直间隔速度的初始估计来调整。 使用在第一层析反转中确定的第二各向异性参数的值,对间隔正常移动速度和相对于深度的第一各向异性参数执行第二断层反演。 再次调整调整后的层深度,间隔正常移动速度和间隔垂直速度,并从第二层析倒置计算间隔椭圆参数。
    • 3. 发明授权
    • Method for three dimensional seismic travel time tomography in transversely isotropic media
    • 横向各向同性介质三维地震行程时间层析成像方法
    • US07663972B2
    • 2010-02-16
    • US12070966
    • 2008-02-22
    • Ruben D. MartinezJunru Jiao
    • Ruben D. MartinezJunru Jiao
    • G01V1/00
    • G01V1/303G01V1/28G01V2210/626G01V2210/66
    • A method for estimating seismic velocities in vertically transversely isotropic media includes generating an initial estimate of vertical interval velocity and interval normal moveout velocity with respect to depth from seismic data. An initial estimate is generated of a first anisotropy parameter with respect to depth. The first anisotropy parameter is related to the interval normal moveout velocity and the interval vertical velocity. An initial estimate is generated with respect to depth of a second anisotropy parameter. The second anisotropy parameter is related to the first anisotropy parameter and an interval anelliptic parameter. A first tomographic inversion is performed with respect to the interval normal moveout velocity and the second anisotropy parameter at a constant value of the first anisotropy parameter until travel time differentials reach minimum values. Layer depths are adjusted with the initial estimate of vertical interval velocity. Using values of the second anisotropy parameter determined in the first tomographic inversion, a second tomographic inversion is performed of interval normal moveout velocity and the first anisotropy parameter with respect to depth. The adjusted layer depths, interval normal moveout velocities and interval vertical velocities are again adjusted and interval anelliptic parameters are calculated from the second tomographic inversion.
    • 用于估计垂直横向各向同性介质中的地震速度的方法包括相对于地震数据的深度产生垂直间隔速度和间隔正常移动速度的初始估计。 产生关于深度的第一各向异性参数的初始估计。 第一个各向异性参数与间隔正常移动速度和间隔垂直速度有关。 相对于第二各向异性参数的深度产生初始估计。 第二个各向异性参数与第一各向异性参数和间隔椭圆参数有关。 在第一各向异性参数的恒定值下,相对于间隔正常移动速度和第二各向异性参数执行第一层析反转,直到行进时间差达到最小值。 层深度用垂直间隔速度的初始估计来调整。 使用在第一层析反转中确定的第二各向异性参数的值,对间隔正常移动速度和相对于深度的第一各向异性参数执行第二断层反演。 再次调整调整后的层深度,间隔正常移动速度和间隔垂直速度,并从第二层析倒置计算间隔椭圆参数。
    • 4. 发明申请
    • Method for building velocity models for imaging in multi-azimuth marine seismic surveys
    • 在多方位角海洋地震勘测中建立成像速度模型的方法
    • US20110292761A1
    • 2011-12-01
    • US12800978
    • 2010-05-27
    • Junru JiaoChaoguang ZhouYeashung Sonny LinSverre Brandsberg-Dahl
    • Junru JiaoChaoguang ZhouYeashung Sonny LinSverre Brandsberg-Dahl
    • G01V1/30G01V1/38
    • G01V1/303
    • A programmable computer is used to perform the following. 3D seismic data sets, corresponding to each azimuth in seismic data obtained from a multi-azimuth marine seismic survey, are migrated in grids oriented with the corresponding azimuth. Acquisition geometry is stored for each trace in the seismic data sets for each azimuth. Residual analysis, based on the corresponding azimuth, is performed on each of the migrated data sets, generating residuals and reflectors for each azimuth. The residuals and reflectors generated for each azimuth are rotated and merged on a master grid. Reflection tomographic inversion is applied iteratively to the rotated and merged residuals and reflectors to update a velocity model using the acquisition geometry as based on the master grid. The earth's subsurface is imaged using the updated velocity model.
    • 可编程计算机用于执行以下操作。 对应于从多方位角海洋地震勘测获得的地震数据中的每个方位角的三维地震数据集,以相应方位定向的网格进行迁移。 为每个方位角的地震数据集中的每个轨迹存储采集几何。 对每个迁移的数据集进行基于相应方位的残差分析,为每个方位角生成残差和反射器。 为每个方位角产生的残差和反射器在主网格上旋转并合并。 反射层析成像反演迭代地应用于旋转和合并的残差和反射器,以使用基于主网格的采集几何来更新速度模型。 使用更新的速度模型对地球的地下成像。
    • 6. 发明授权
    • Method for building velocity models for imaging in multi-azimuth marine seismic surveys
    • 在多方位角海洋地震勘测中建立成像速度模型的方法
    • US08908471B2
    • 2014-12-09
    • US12800978
    • 2010-05-27
    • Junru JiaoChaoguang ZhouYeashung Sonny LinSverre Brandsberg-Dahl
    • Junru JiaoChaoguang ZhouYeashung Sonny LinSverre Brandsberg-Dahl
    • G01V1/38G01V1/30
    • G01V1/303
    • A programmable computer is used to perform the following. 3D seismic data sets, corresponding to each azimuth in seismic data obtained from a multi-azimuth marine seismic survey, are migrated in grids oriented with the corresponding azimuth. Acquisition geometry is stored for each trace in the seismic data sets for each azimuth. Residual analysis, based on the corresponding azimuth, is performed on each of the migrated data sets, generating residuals and reflectors for each azimuth. The residuals and reflectors generated for each azimuth are rotated and merged on a master grid. Reflection tomographic inversion is applied iteratively to the rotated and merged residuals and reflectors to update a velocity model using the acquisition geometry as based on the master grid. The earth's subsurface is imaged using the updated velocity model.
    • 可编程计算机用于执行以下操作。 对应于从多方位角海洋地震勘测获得的地震数据中的每个方位角的三维地震数据集在以相应方位定向的网格中迁移。 为每个方位角的地震数据集中的每个轨迹存储采集几何。 对每个迁移的数据集进行基于相应方位的残差分析,为每个方位角生成残差和反射器。 为每个方位角产生的残差和反射器在主网格上旋转并合并。 反射层析成像反演迭代地应用于旋转和合并的残差和反射器,以使用基于主网格的采集几何来更新速度模型。 使用更新的速度模型对地球的地下成像。