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1. 发明授权

US08428925B2 Iterative inversion of data from simultaneous geophysical sources 有权
标题翻译：同时地球物理资料数据的迭代反演
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）。

2. 发明申请

US20120109612A1 Iterative Inversion of Data From Simultaneous Geophysical Sources 有权
标题翻译：同时地球物理资料的迭代反演数据
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）。

3. 发明申请

US20100018718A1 ITERATIVE INVERSION OF DATA FROM SIMULTANEOUS GEOPHYSICAL SOURCES 有权
标题翻译：数据同源地球物理资料的迭代反演
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
IPC分类号： E21B43/00 , G01V1/28 , G06F19/00
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）。

4. 发明授权

US08537638B2 Methods for subsurface parameter estimation in full wavefield inversion and reverse-time migration 有权
标题翻译：全波场反演和反向时间迁移的地下参数估计方法
公开(公告)号：US08537638B2
公开(公告)日：2013-09-17
申请号：US12984412
申请日：2011-01-04
申请人： Sunwoong Lee , Jerome R. Krebs , John E. Anderson , Anatoly Baumstein , David L. Hinkley
发明人： Sunwoong Lee , Jerome R. Krebs , John E. Anderson , Anatoly Baumstein , David L. Hinkley
IPC分类号： G01V1/00 , G01V1/28
CPC分类号： G01V1/00 , G01V1/28 , G01V1/282 , G01V1/301 , G01V1/306 , G01V1/368 , G01V2210/51 , G01V2210/614 , G01V2210/622 , G01V2210/663 , G01V2210/675 , G01V2210/679
摘要： Method for converting seismic data to obtain a subsurface model of, for example, bulk modulus or density. The gradient of an objective function is computed (103) using the seismic data (101) and a background subsurface medium model (102). The source and receiver illuminations are computed in the background model (104). The seismic resolution volume is computed using the velocities of the background model (105). The gradient is converted into the difference subsurface model parameters (106) using the source and receiver illumination, seismic resolution volume, and the background subsurface model. These same factors may be used to compensate seismic data migrated by reverse time migration, which can then be related to a subsurface bulk modulus model. For iterative inversion, the difference subsurface model parameters (106) are used as preconditioned gradients (107).
摘要翻译：用于转换地震数据以获得例如体积模量或密度的地下模型的方法。使用地震数据（101）和背景地下介质模型（102）计算目标函数的梯度（103）。源和接收器照明在背景模型（104）中计算。使用背景模型（105）的速度计算地震解析度。使用源和接收器照明，地震分辨率体积和背景地下模型将梯度转换为差分地下模型参数（106）。这些相同的因素可以用于补偿通过反向时间迁移迁移的地震数据，其然后可以与地下体积模量模型相关。对于迭代反演，差分地下模型参数（106）用作预处理梯度（107）。

5. 发明授权

US08223587B2 Full wavefield inversion using time varying filters 有权
标题翻译：使用时变滤波器的全波场反演
公开(公告)号：US08223587B2
公开(公告)日：2012-07-17
申请号：US13020502
申请日：2011-02-03
申请人： Jerome R. Krebs , John E. Anderson
发明人： Jerome R. Krebs , John E. Anderson
IPC分类号： G01V1/00 , G06F17/20
CPC分类号： G01V1/282
摘要： An improved method for reducing the accuracy requirements on the starting model when performing multi-scale inversion of seismic data (65) by local objective function optimization (64). The different scales of inversion are brought about by incorporating a low-pass filter into the objective function (61), and then decreasing the amount of high-frequency data that is filtered out from one scale to the next. Moreover, the filter is designed to be time varying, wherein the filter's low-pass cutoff frequency decreases with increasing traveltime of the seismic data being filtered (62). The filter may be designed using Pratt's criterion for eliminating local minima, and performing averages (or other statistical measure) of the period and the traveltime error only with respect to source and receiver location but not traveltime (63).
摘要翻译：（65）通过局部目标函数优化（64）对地震数据进行多尺度反演（65）时，降低起始模型精度要求的改进方法。通过将低通滤波器合并到目标函数（61）中，然后将从一个比例过滤出的高频数据的量减少到下一个尺度，从而产生不同的反演尺度。此外，滤波器被设计为时变的，其中滤波器的低通截止频率随着被过滤的地震数据的行进时间的增加而减小（62）。滤波器可以使用Pratt的标准来设计，用于消除局部最小值，并且仅针对源和接收器位置而不是行进时间执行周期的平均值（或其他统计测量）和行进时间误差（63）。

6. 发明申请

US20130191090A1 Iterative Inversion of Data from Simultaneous Geophysical Sources 审中-公开
标题翻译：同时地球物理资料数据迭代反演
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）。

7. 发明授权

US08121823B2 Iterative inversion of data from simultaneous geophysical sources 有权
标题翻译：同时地球物理资料数据的迭代反演
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）。

8. 发明申请

US20110238390A1 Full Wavefield Inversion Using Time Varying Filters 有权
标题翻译：使用时变滤波器的全波场反演
公开(公告)号：US20110238390A1
公开(公告)日：2011-09-29
申请号：US13020502
申请日：2011-02-03
申请人： Jerome R. Krebs , John E. Anderson
发明人： Jerome R. Krebs , John E. Anderson
IPC分类号： G06F17/10
CPC分类号： G01V1/282
摘要： An improved method for reducing the accuracy requirements on the starting model when performing multi-scale inversion of seismic data (65) by local objective function optimization (64). The different scales of inversion are brought about by incorporating a low-pass filter into the objective function (61), and then decreasing the amount of high-frequency data that is filtered out from one scale to the next. Moreover, the filter is designed to be time varying, wherein the filter's low-pass cutoff frequency decreases with increasing traveltime of the seismic data being filtered (62). The filter may be designed using Pratt's criterion for eliminating local minima, and performing averages (or other statistical measure) of the period and the traveltime error only with respect to source and receiver location but not traveltime (63).
摘要翻译：（65）通过局部目标函数优化（64）对地震数据进行多尺度反演（65）时，降低起始模型精度要求的改进方法。通过将低通滤波器合并到目标函数（61）中，然后将从一个比例过滤出的高频数据的量减少到下一个尺度，从而产生不同的反演尺度。此外，滤波器被设计为时变的，其中滤波器的低通截止频率随着被过滤的地震数据的行进时间的增加而减小（62）。滤波器可以使用Pratt的标准来设计，用于消除局部最小值，并且仅针对源和接收器位置而不是行进时间执行周期的平均值（或其他统计测量）和行进时间误差（63）。

9. 发明申请

US20110194379A1 Methods For Subsurface Parameter Estimation In Full Wavefield Inversion And Reverse-Time Migration 有权
标题翻译：全波场反演和反向时间迁移的地下参数估计方法
公开(公告)号：US20110194379A1
公开(公告)日：2011-08-11
申请号：US12984412
申请日：2011-01-04
申请人： Sunwoong Lee , Jerome R. Krebs , John E. Anderson , Anatoly Baumstein , David L. Hinkley
发明人： Sunwoong Lee , Jerome R. Krebs , John E. Anderson , Anatoly Baumstein , David L. Hinkley
IPC分类号： G01V1/28
CPC分类号： G01V1/00 , G01V1/28 , G01V1/282 , G01V1/301 , G01V1/306 , G01V1/368 , G01V2210/51 , G01V2210/614 , G01V2210/622 , G01V2210/663 , G01V2210/675 , G01V2210/679
摘要： Method for converting seismic data to obtain a subsurface model of, for example, bulk modulus or density. The gradient of an objective function is computed (103) using the seismic data (101) and a background subsurface medium model (102). The source and receiver illuminations are computed in the background model (104). The seismic resolution volume is computed using the velocities of the background model (105). The gradient is converted into the difference subsurface model parameters (106) using the source and receiver illumination, seismic resolution volume, and the background subsurface model. These same factors may be used to compensate seismic data migrated by reverse time migration, which can then be related to a subsurface bulk modulus model. For iterative inversion, the difference subsurface model parameters (106) are used as preconditioned gradients (107).
摘要翻译：用于转换地震数据以获得例如体积模量或密度的地下模型的方法。使用地震数据（101）和背景地下介质模型（102）计算目标函数的梯度（103）。源和接收器照明在背景模型（104）中计算。使用背景模型（105）的速度计算地震解析度。使用源和接收器照明，地震分辨率体积和背景地下模型将梯度转换为差分地下模型参数（106）。这些相同的因素可以用于补偿通过反向时间迁移迁移的地震数据，其然后可以与地下体积模量模型相关。对于迭代反演，差分地下模型参数（106）用作预处理梯度（107）。

10. 发明授权

US10768325B2 Method to estimate 4D seismic acquisition repeatability specifications from high-resolution near-water-bottom seismic images 有权
公开(公告)号：US10768325B2
公开(公告)日：2020-09-08
申请号：US15722638
申请日：2017-10-02
申请人： Norman C. Allegar , John E. Anderson , Simon Dewing
发明人： Norman C. Allegar , John E. Anderson , Simon Dewing
IPC分类号： G01V1/30 , G01V1/38
摘要： A method for designing 4-D seismic acquisition source and receiver repeatability specifications, the method including: locating, with a computer subsurface anomalies above a target reservoir zone from analysis of high-resolution reflectivity images for the target reservoir zone; determining, with a computer, how the anomalies above the target reservoir zone modify target illumination for variations in the 4-D seismic acquisition source and receiver positions; and determining, with a computer, repeatability specifications for a monitor seismic survey, wherein tolerances for the source or receiver positions varies across an acquisition area based on how the anomalies modify the target illumination.

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