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公开(公告)号：US08121823B2
公开(公告)日：2012-02-21
申请号：US12441685
申请日：2007-09-11
申请人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charlie Jing , David Hinkley , Thomas A. Dickens , Christine E. Krohn , Peter Traynin
发明人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charlie Jing , David Hinkley , Thomas A. Dickens , Christine E. Krohn , Peter Traynin
IPC分类号： G06G7/48
CPC分类号： G06F17/5009 , G01V1/28 , G01V2210/67
摘要： Method for reducing the time needed to perform geophysical inversion by using simultaneous encoded sources in the simulation steps of the inversion process. The geophysical survey data are prepared by encoding (3) a group of source gathers (1), using for each gather a different encoding signature selected from a set (2) of non-equivalent encoding signatures. Then, the encoded gathers are summed (4) by summing all traces corresponding to the same receiver from each gather, resulting in a simultaneous encoded gather. (Alternatively, the geophysical data are acquired from simultaneously encoded sources.) The simulation steps needed for inversion are then calculated using a particular assumed velocity (or other physical property) model (5) and simultaneously activated encoded sources using the same encoding scheme used on the measured data. The result is an updated physical properties model (6) that may be further updated (7) by additional iterations.
摘要翻译： 用于在反演过程的仿真步骤中通过使用同时编码的源来减少执行地球物理反演所需的时间的方法。 通过编码（3）一组源集合（1）来准备地球物理勘测数据，使用每组收集从非等效编码签名集合（2）中选出的不同编码签名。 然后，通过将来自每个聚集的相同接收器的所有跟踪相加，将编码的聚集相加（4），导致同时编码的聚集。 （或者，从同时编码的源获取地球物理数据。）然后使用特定的假定速度（或其他物理属性）模型（5）计算反演所需的模拟步骤，并使用与之相同的编码方案同时激活编码的源 测量数据。 结果是可以通过附加迭代进一步更新（7）的更新的物理属性模型（6）。
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公开(公告)号：US08428925B2
公开(公告)日：2013-04-23
申请号：US13345314
申请日：2012-01-06
申请人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charlie Jing , David Hinkley , Thomas A. Dickens , Christine E. Krohn , Peter Traynin
发明人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charlie Jing , David Hinkley , Thomas A. Dickens , Christine E. Krohn , Peter Traynin
IPC分类号： G06G7/48
CPC分类号： G06F17/5009 , G01V1/28 , G01V2210/67
摘要： Method for reducing the time needed to perform geophysical inversion by using simultaneous encoded sources in the simulation steps of the inversion process. The geophysical survey data are prepared by encoding (3) a group of source gathers (1), using for each gather a different encoding signature selected from a set (2) of non-equivalent encoding signatures. Then, the encoded gathers are summed (4) by summing all traces corresponding to the same receiver from each gather, resulting in a simultaneous encoded gather. (Alternatively, the geophysical data are acquired from simultaneously encoded sources.) The simulation steps needed for inversion are then calculated using a particular assumed velocity (or other physical property) model (5) and simultaneously activated encoded sources using the same encoding scheme used on the measured data. The result is an updated physical properties model (6) that may be further updated (7) by additional iterations.
摘要翻译： 用于在反演过程的仿真步骤中通过使用同时编码的源来减少执行地球物理反演所需的时间的方法。 通过编码（3）一组源集合（1）来准备地球物理勘测数据，使用每组收集从非等效编码签名集合（2）中选出的不同编码签名。 然后，通过将来自每个聚集的相同接收器的所有跟踪相加，将编码的聚集相加（4），导致同时编码的聚集。 （或者，从同时编码的源获取地球物理数据。）然后使用特定的假定速度（或其他物理属性）模型（5）计算反演所需的模拟步骤，并使用与之相同的编码方案同时激活编码的源 测量数据。 结果是可以通过附加迭代进一步更新（7）的更新的物理属性模型（6）。
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公开(公告)号：US20120109612A1
公开(公告)日：2012-05-03
申请号：US13345314
申请日：2012-01-06
申请人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charlie Jing , David Hinkley , Thomas A. Dickens , Christine E. Krohn , Peter Traynin
发明人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charlie Jing , David Hinkley , Thomas A. Dickens , Christine E. Krohn , Peter Traynin
IPC分类号： G06G7/48
CPC分类号： G06F17/5009 , G01V1/28 , G01V2210/67
摘要： Method for reducing the time needed to perform geophysical inversion by using simultaneous encoded sources in the simulation steps of the inversion process. The geophysical survey data are prepared by encoding (3) a group of source gathers (1), using for each gather a different encoding signature selected from a set (2) of non-equivalent encoding signatures. Then, the encoded gathers are summed (4) by summing all traces corresponding to the same receiver from each gather, resulting in a simultaneous encoded gather. (Alternatively, the geophysical data are acquired from simultaneously encoded sources.) The simulation steps needed for inversion are then calculated using a particular assumed velocity (or other physical property) model (5) and simultaneously activated encoded sources using the same encoding scheme used on the measured data. The result is an updated physical properties model (6) that may be further updated (7) by additional iterations.
摘要翻译： 用于在反演过程的仿真步骤中通过使用同时编码的源来减少执行地球物理反演所需的时间的方法。 通过编码（3）一组源集合（1）来准备地球物理勘测数据，使用每组收集从非等效编码签名集合（2）中选出的不同编码签名。 然后，通过将来自每个聚集的相同接收器的所有跟踪相加，将编码的聚集相加（4），导致同时编码的聚集。 （或者，从同时编码的源获得地球物理数据。）然后使用特定的假定速度（或其他物理属性）模型（5）计算反演所需的模拟步骤，并使用与之相同的编码方案同时激活编码的源 测量数据。 结果是可以通过附加迭代进一步更新（7）的更新的物理属性模型（6）。
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公开(公告)号：US20100018718A1
公开(公告)日：2010-01-28
申请号：US12441685
申请日：2007-09-11
申请人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charlie Jing , David Hinkley , Thomas A. Dickens , Christine E. Krohn , Peter Traynin
发明人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charlie Jing , David Hinkley , Thomas A. Dickens , Christine E. Krohn , Peter Traynin
CPC分类号： G06F17/5009 , G01V1/28 , G01V2210/67
摘要： Method for reducing the time needed to perform geophysical inversion by using simultaneous encoded sources in the simulation steps of the inversion process. The geophysical survey data are prepared by encoding (3) a group of source gathers (1), using for each gather a different encoding signature selected from a set (2) of non-equivalent encoding signatures. Then, the encoded gathers are summed (4) by summing all traces corresponding to the same receiver from each gather, resulting in a simultaneous encoded gather (Alternatively, the geophysical data are acquired from simultaneously encoded sources.) The simulation steps needed for inversion are then calculated using a particular assumed velocity (or other physical property) model (5) and simultaneously activated encoded sources using the same encoding scheme used on the measured data. The result is an updated physical properties model (6) that may be further updated (7) by additional iterations.
摘要翻译： 用于在反演过程的仿真步骤中通过使用同时编码的源来减少执行地球物理反演所需的时间的方法。 通过编码（3）一组源集合（1）来准备地球物理勘测数据，使用每组收集从非等效编码签名集合（2）中选出的不同编码签名。 然后，通过对来自每个聚集的相同接收器的所有跟踪进行求和，将编码的聚集相加（4），导致同时编码的聚集（或者，从同时编码的源获取地球物理数据）。反演所需的模拟步骤是 然后使用特定的假定速度（或其他物理属性）模型（5）计算，并使用与测量数据相同的编码方案同时激活编码的源。 结果是可以通过附加迭代进一步更新（7）的更新的物理属性模型（6）。
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公开(公告)号：US20130191090A1
公开(公告)日：2013-07-25
申请号：US13791252
申请日：2013-03-08
申请人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charles Jing , David L. Hinkley , Thomas A. Dickens
发明人： Jerome R. Krebs , John E. Anderson , Ramesh Neelamani , Charles Jing , David L. Hinkley , Thomas A. Dickens
IPC分类号： G06F17/50
CPC分类号： G06F17/5009 , G01V1/28 , G01V2210/67
摘要： Method for reducing the time needed to perform geophysical inversion by using simultaneous encoded sources in the simulation steps of the inversion process. The geophysical survey data are prepared by encoding (3) a group of source gathers (1), using for each gather a different encoding signature selected from a set (2) of non-equivalent encoding signatures. Then, the encoded gathers are summed (4) by summing all traces corresponding to the same receiver from each gather, resulting in a simultaneous encoded gather. (Alternatively, the geophysical data are acquired from simultaneously encoded sources.) The simulation steps needed for inversion are then calculated using a particular assumed velocity (or other physical property) model (5) and simultaneously activated encoded sources using the same encoding scheme used on the measured data. The result is an updated physical properties model (6) that may be further updated (7) by additional iterations.
摘要翻译： 用于在反演过程的仿真步骤中通过使用同时编码的源来减少执行地球物理反演所需的时间的方法。 通过编码（3）一组源集合（1）来准备地球物理勘测数据，使用每组收集从非等效编码签名集合（2）中选出的不同编码签名。 然后，通过将来自每个聚集的相同接收器的所有跟踪相加，将编码的聚集相加（4），导致同时编码的聚集。 （或者，从同时编码的源获取地球物理数据。）然后使用特定的假定速度（或其他物理属性）模型（5）计算反演所需的模拟步骤，并使用与之相同的编码方案同时激活编码的源 测量数据。 结果是可以通过附加迭代进一步更新（7）的更新的物理属性模型（6）。
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公开(公告)号：US20130003500A1
公开(公告)日：2013-01-03
申请号：US13614932
申请日：2012-09-13
申请人： Ramesh Neelamani , Partha S. Routh , Jerome R. Krebs , Anatoly Baumstein , Thomas A. Dickens , Warren S. Ross , Gopalkrishna Palacharla
发明人： Ramesh Neelamani , Partha S. Routh , Jerome R. Krebs , Anatoly Baumstein , Thomas A. Dickens , Warren S. Ross , Gopalkrishna Palacharla
IPC分类号： G01V1/28
CPC分类号： G01V1/28 , G01V2210/32 , G01V2210/40 , G01V2210/51
摘要： The invention includes a method for reducing noise in migration of seismic data, particularly advantageous for imaging by simultaneous encoded source reverse-time migration (SS-RTM). One example embodiment includes the steps of obtaining a plurality of initial subsurface images; decomposing each of the initial subsurface images into components; identifying a set of components comprising one of (i) components having at least one substantially similar characteristic across the plurality of initial subsurface images, and (ii) components having substantially dissimilar characteristics across the plurality of initial subsurface images; and generating an enhanced subsurface image using the identified set of components. For SS-RTM, each of the initial subsurface images is generated by migrating several sources simultaneously using a unique random set of encoding functions. Another embodiment of the invention uses SS-RTM for velocity model building.
摘要翻译： 本发明包括一种降低地震数据迁移噪声的方法，特别有利于通过同时编码的源反向时间迁移（SS-RTM）进行成像。 一个示例实施例包括获得多个初始地下图像的步骤; 将每个初始地下图像分解成分量; 识别包括（i）在所述多个初始地下图像中具有至少一个基本上相似的特征的分量之一的组件集合;以及（ii）在所述多个初始地下图像之间具有基本不相似特征的分量; 以及使用所识别的组件集合来生成增强的地下图像。 对于SS-RTM，每个初始地下图像都是通过使用唯一随机的编码函数集同时迁移多个源来生成的。 本发明的另一个实施例使用SS-RTM进行速度模型建立。
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公开(公告)号：US20120275267A1
公开(公告)日：2012-11-01
申请号：US13430380
申请日：2012-03-26
IPC分类号： G01V1/28
CPC分类号： G01V1/28 , G01V2210/51
摘要： Provided is a method for processing seismic data. One exemplary embodiment includes the steps of obtaining a plurality of initial subsurface images; decomposing each of the initial subsurface images into components; identifying a set of components comprising one of (i) components having at least one substantially similar characteristic across the plurality of initial subsurface images, and (ii) components having substantially dissimilar characteristics across the plurality of initial subsurface images; and generating an enhanced subsurface image using the identified set of components. Each of the initial subsurface images is generated using a unique random set of encoding functions.
摘要翻译： 提供了一种处理地震数据的方法。 一个示例性实施例包括获得多个初始地下图像的步骤; 将每个初始地下图像分解成分量; 识别包括（i）在所述多个初始地下图像中具有至少一个基本上相似的特征的分量之一的组件集合;以及（ii）在所述多个初始地下图像之间具有基本不相似特征的分量; 以及使用所识别的组件集合来生成增强的地下图像。 使用唯一随机的编码函数集来生成每个初始地下图像。
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公开(公告)号：US09625593B2
公开(公告)日：2017-04-18
申请号：US13614932
申请日：2012-09-13
申请人： Ramesh Neelamani , Partha S. Routh , Jerome R. Krebs , Anatoly Baumstein , Thomas A. Dickens , Warren S. Ross , Gopalkrishna Palacharla
发明人： Ramesh Neelamani , Partha S. Routh , Jerome R. Krebs , Anatoly Baumstein , Thomas A. Dickens , Warren S. Ross , Gopalkrishna Palacharla
IPC分类号： G01V1/28
CPC分类号： G01V1/28 , G01V2210/32 , G01V2210/40 , G01V2210/51
摘要： The invention includes a method for reducing noise in migration of seismic data, particularly advantageous for imaging by simultaneous encoded source reverse-time migration (SS-RTM). One example embodiment includes the steps of obtaining a plurality of initial subsurface images; decomposing each of the initial subsurface images into components; identifying a set of components comprising one of (i) components having at least one substantially similar characteristic across the plurality of initial subsurface images, and (ii) components having substantially dissimilar characteristics across the plurality of initial subsurface images; and generating an enhanced subsurface image using the identified set of components. For SS-RTM, each of the initial subsurface images is generated by migrating several sources simultaneously using a unique random set of encoding functions. Another embodiment of the invention uses SS-RTM for velocity model building.
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9.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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10.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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