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1.发明申请Simultaneous Source Encoding and Source Separation As A Practical Solution For Full Wavefield Inversion 有权同源信源编码和源分离作为全波场反演的实际解决方案公开(公告)号：US20120073825A1
公开(公告)日：2012-03-29
申请号：US13229252
申请日：2011-09-09
申请人： Partha S. Routh , Sunwoong Lee , Ramesh Neelamani , Jerome R. Krebs , Spyridon Lazaratos , Carey Marcinkovich
发明人： Partha S. Routh , Sunwoong Lee , Ramesh Neelamani , Jerome R. Krebs , Spyridon Lazaratos , Carey Marcinkovich
CPC分类号： G01V1/28 , G01V2210/67
摘要： Method for simultaneous full-wavefield inversion of gathers of source (or receiver) encoded geophysical data to determine a physical properties model (118) for a subsurface region, especially suitable for surveys where fixed receiver geometry conditions were not satisfied in the data acquisition. Simultaneous source separation (104) is performed to lessen any effect of the measured geophysical data's not satisfying the fixed-receiver assumption. A data processing step (106) coming after the simultaneous source separation acts to conform model-simulated data (105) to the measured geophysical data (108) for source and receiver combinations that are missing in the measured geophysical data.
摘要翻译： 用于同源全波场反演源（或接收机）编码的地球物理数据的方法，以确定地下区域的物理性质模型（118），特别适合于在数据采集中不满足固定接收机几何条件的调查。 执行同源分离（104）以减少测量的地球物理数据不满足固定接收机假设的任何影响。 在同时源分离之后进行的数据处理步骤（106）用于将模拟模拟数据（105）符合测量的地球物理数据（108），用于测量的地球物理数据中缺少的源和接收机组合。
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2.发明授权Hybrid method for full waveform inversion using simultaneous and sequential source method 有权使用同步和顺序源方法进行全波形反演的混合方法公开(公告)号：US08437998B2
公开(公告)日：2013-05-07
申请号：US12903744
申请日：2010-10-13
IPC分类号： G06G7/48
CPC分类号： G01V1/28 , G01V1/005 , G01V2210/67
摘要： Method for simultaneous full-wavefield inversion of gathers of source (or receiver) encoded geophysical data to determine a physical properties model for a subsurface region, especially suitable for surveys where fixed receiver geometry conditions were not satisfied in the data acquisition. First, a shallow time window of the data (202) where the fixed receiver condition is satisfied is inverted by simultaneous encoded (203) source inversion (205). Then, the deeper time window of the data (208) is inverted by sparse sequential source inversion (209), using the physical properties model from the shallow time window (206) as a starting model (207). Alternatively, the shallow time window model is used to simulate missing far offset data (211) producing a data set satisfying the stationary receiver assumption, after which this data set is source encoded (212) and inverted by simultaneous source inversion (214).
摘要翻译： 源（或接收机）编码地球物理数据的同时全波场反演方法，以确定地下区域的物理性质模型，特别适用于在数据采集中不满足固定接收机几何条件的调查。 首先，通过同时编码（203）源反转（205）来反转其中满足固定接收机条件的数据（202）的浅时间窗口。 然后，使用来自浅时间窗口（206）的物理属性模型作为起始模型（207），通过稀疏顺序源反转（209）将数据（208）的更深的时间窗口反转。 或者，浅时间窗模型用于模拟产生满足固定接收机假设的数据集的丢失远偏移数据（211），之后该数据集被源编码（212）并且由同时源反转（214）反转。
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3.发明授权Simultaneous source encoding and source separation as a practical solution for full wavefield inversion 有权同源源编码和源分离作为全波场反演的实际解决方案公开(公告)号：US08775143B2
公开(公告)日：2014-07-08
申请号：US13229252
申请日：2011-09-09
申请人： Partha S. Routh , Sunwoong Lee , Ramesh Neelamani , Jerome R. Krebs , Spyridon Lazaratos , Carey Marcinkovich
发明人： Partha S. Routh , Sunwoong Lee , Ramesh Neelamani , Jerome R. Krebs , Spyridon Lazaratos , Carey Marcinkovich
IPC分类号： G06G7/48
CPC分类号： G01V1/28 , G01V2210/67
摘要： Method for simultaneous full-wavefield inversion of gathers of source (or receiver) encoded geophysical data to determine a physical properties model (118) for a subsurface region, especially suitable for surveys where fixed receiver geometry conditions were not satisfied in the data acquisition. Simultaneous source separation (104) is performed to lessen any effect of the measured geophysical data's not satisfying the fixed-receiver assumption. A data processing step (106) coming after the simultaneous source separation acts to conform model-simulated data (105) to the measured geophysical data (108) for source and receiver combinations that are missing in the measured geophysical data.
摘要翻译： 用于同源全波场反演源（或接收机）编码的地球物理数据的方法，以确定地下区域的物理性质模型（118），特别适合于在数据采集中不满足固定接收机几何条件的调查。 执行同源分离（104）以减少测量的地球物理数据不满足固定接收机假设的任何影响。 在同时源分离之后进行的数据处理步骤（106）用于将模拟模拟数据（105）符合测量的地球物理数据（108），用于测量的地球物理数据中缺少的源和接收机组合。
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4.发明申请Hybride Method For Full Waveform Inversion Using Simultaneous and Sequential Source Method 有权使用同时和顺序源方法进行全波形反演的Hybride方法公开(公告)号：US20120073824A1
公开(公告)日：2012-03-29
申请号：US12903744
申请日：2010-10-13
CPC分类号： G01V1/28 , G01V1/005 , G01V2210/67
摘要： Method for simultaneous full-wavefield inversion of gathers of source (or receiver) encoded geophysical data to determine a physical properties model for a subsurface region, especially suitable for surveys where fixed receiver geometry conditions were not satisfied in the data acquisition. First, a shallow time window of the data (202) where the fixed receiver condition is satisfied is inverted by simultaneous encoded (203) source inversion (205). Then, the deeper time window of the data (208) is inverted by sparse sequential source inversion (209), using the physical properties model from the shallow time window (206) as a starting model (207). Alternatively, the shallow time window model is used to simulate missing far offset data (211) producing a data set satisfying the stationary receiver assumption, after which this data set is source encoded (212) and inverted by simultaneous source inversion (214).
摘要翻译： 源（或接收机）编码地球物理数据的同时全波场反演方法，以确定地下区域的物理性质模型，特别适用于在数据采集中不满足固定接收机几何条件的调查。 首先，通过同时编码（203）源反转（205）来反转其中满足固定接收机条件的数据（202）的浅时间窗口。 然后，使用来自浅时间窗口（206）的物理属性模型作为起始模型（207），通过稀疏顺序源反转（209）将数据（208）的更深的时间窗口反转。 或者，浅时间窗模型用于模拟产生满足固定接收机假设的数据集的丢失远偏移数据（211），之后该数据集被源编码（212）并且由同时源反转（214）反转。
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5.发明授权Simultaneous source inversion for marine streamer data with cross-correlation objective function 有权具有互相关目标函数的海洋流光数据同时源反演公开(公告)号：US08688381B2
公开(公告)日：2014-04-01
申请号：US13224005
申请日：2011-09-01
IPC分类号： G06F19/00
摘要： Method for simultaneous full-wavefield inversion of gathers of source (or receiver) encoded (30) geophysical data (80) to determine a physical properties model (20) for a subsurface region, especially suitable for surveys where fixed-receiver geometry conditions were not satisfied in the data acquisition (40). The inversion involves optimization of a cross-correlation objective function (100).
摘要翻译： 源（或接收器）编码（30）地球物理数据（80）的聚集的同时全波场反演的方法，以确定地下区域的物理性质模型（20），特别适用于固定接收机几何条件不是的调查 满意的数据采集（40）。 反演涉及互相关目标函数的优化（100）。
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6.发明申请Simultaneous Source Inversion for Marine Streamer Data With Cross-Correlation Objective Function 有权海洋流光数据与交叉相关目标函数的同时源反演公开(公告)号：US20120143506A1
公开(公告)日：2012-06-07
申请号：US13224005
申请日：2011-09-01
IPC分类号： G06F19/00
摘要： Method for simultaneous full-wavefield inversion of gathers of source (or receiver) encoded (30) geophysical data (80) to determine a physical properties model (20) for a subsurface region, especially suitable for surveys where fixed-receiver geometry conditions were not satisfied in the data acquisition (40). The inversion involves optimization of a cross-correlation objective function (100).
摘要翻译： 源（或接收器）编码（30）地球物理数据（80）的聚集的同时全波场反演的方法，以确定地下区域的物理性质模型（20），特别适用于固定接收机几何条件不是的调查 满意的数据采集（40）。 反演涉及互相关目标函数的优化（100）。
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公开(公告)号：US20140350861A1
公开(公告)日：2014-11-27
申请号：US14272020
申请日：2014-05-07
申请人： Ke Wang , Spyridon Lazaratos
发明人： Ke Wang , Spyridon Lazaratos
IPC分类号： G01V1/28
CPC分类号： G01V1/28 , G01V1/303 , G01V1/306 , G01V2210/622 , G01V2210/673
摘要： Method for multi-parameter inversion using elastic inversion. This method decomposes data into offset/angle groups and performs inversion on them in sequential order. This method can significantly speed up convergence of the iterative inversion process, and is therefore most advantageous when used for full waveform inversion (FWI). The present inventive approach draws upon relationships between reflection energy and reflection angle, or equivalently, offset dependence in elastic FWI. The invention uses recognition that the amplitudes of small angle (near offset) reflections are largely determined by acoustic impedance alone (1), independent for the most part of Vp/Vs. Large angle (middle and far offset) reflections are affected by Ip, Vp/Vs (2) and other earth parameters such as density (3) and anisotropy. Therefore, the present inventive method decomposes data into angle or offset groups in performing multi-parameter FWI to reduce crosstalk between the different model parameters being determined in the inversion.
摘要翻译： 使用弹性反演的多参数反演方法。 该方法将数据分解为偏移/角度组，并按顺序执行反演。 这种方法可以显着加快迭代反演过程的收敛，因此当用于全波形反演（FWI）时最有利。 本发明的方法利用反射能量和反射角度之间的关系，或等效地，弹性FWI中的偏移依赖性。 本发明使用识别，小角度（近偏移）反射的幅度主要由声阻抗单独确定（1），对于大部分Vp / Vs而言是独立的。 大角度（中，远偏移）反射受Ip，Vp / Vs（2）和其他地球参数如密度（3）和各向异性的影响。 因此，本发明的方法在执行多参数FWI时将数据分解为角度或偏移组，以减少在反演中确定的不同模型参数之间的串扰。
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公开(公告)号：US09702993B2
公开(公告)日：2017-07-11
申请号：US14272020
申请日：2014-05-07
申请人： Ke Wang , Spyridon Lazaratos
发明人： Ke Wang , Spyridon Lazaratos
CPC分类号： G01V1/28 , G01V1/303 , G01V1/306 , G01V2210/622 , G01V2210/673
摘要： Method for multi-parameter inversion using elastic inversion. This method decomposes data into offset/angle groups and performs inversion on them in sequential order. This method can significantly speed up convergence of the iterative inversion process, and is therefore most advantageous when used for full waveform inversion (FWI). The present inventive approach draws upon relationships between reflection energy and reflection angle, or equivalently, offset dependence in elastic FWI. The invention uses recognition that the amplitudes of small angle (near offset) reflections are largely determined by acoustic impedance alone (1), independent for the most part of Vp/Vs. Large angle (middle and far offset) reflections are affected by Ip, Vp/Vs (2) and other earth parameters such as density (3) and anisotropy. Therefore, the present inventive method decomposes data into angle or offset groups in performing multi-parameter FWI to reduce crosstalk between the different model parameters being determined in the inversion.
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公开(公告)号：US08121791B2
公开(公告)日：2012-02-21
申请号：US12742561
申请日：2008-12-05
申请人： Spyridon Lazaratos , Roy L. David
发明人： Spyridon Lazaratos , Roy L. David
IPC分类号： G06F17/14
CPC分类号： G01V1/36 , G01V2210/51 , G01V2210/67
摘要： A geophysical model of a subsurface region is generated based on seismic data, e.g., seismic reflection data. Migration and seismic inversion are applied to the seismic data to generate estimates of one or more physical or seismic properties of the subsurface region. Seismic inversion, such as spectral shaping inversion, is applied before or after migrating the seismic data through a variety of techniques that each avoid the amplification of dipping energy while optimizing computational efficiency and/or accuracy.
摘要翻译： 基于地震数据（例如地震反射数据）生成地下区域的地球物理模型。 移动和地震反演应用于地震数据，以产生地下区域的一个或多个物理或地震属性的估计。 在通过各种避免浸渍能量放大同时优化计算效率和/或准确度的各种技术迁移地震数据之前或之后，应用地震反演，例如频谱整形反演。
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公开(公告)号：US20100270026A1
公开(公告)日：2010-10-28
申请号：US12742561
申请日：2008-12-05
申请人： Spyridon Lazaratos , Roy David
发明人： Spyridon Lazaratos , Roy David
CPC分类号： G01V1/36 , G01V2210/51 , G01V2210/67
摘要： A geophysical model of a subsurface region is generated based on seismic data, e.g., seismic reflection data. Migration and seismic inversion are applied to the seismic data to generate estimates of one or more physical or seismic properties of the subsurface region. Seismic inversion, such as spectral shaping inversion, is applied before or after migrating the seismic data through a variety of techniques that each avoid the amplification of dipping energy while optimizing computational efficiency and/or accuracy.
摘要翻译： 基于地震数据（例如地震反射数据）生成地下区域的地球物理模型。 移动和地震反演应用于地震数据，以产生地下区域的一个或多个物理或地震属性的估计。 在通过各种避免浸渍能量放大同时优化计算效率和/或准确度的各种技术迁移地震数据之前或之后，应用地震反演，例如频谱整形反演。
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