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1.发明申请Method For Geophysical and Geological Interpretation of Seismic Volumes In The Domains of Depth, Time, and Age 审中-公开深度，时间和年龄域地震卷的地球物理和地质解释方法公开(公告)号：US20100149917A1
公开(公告)日：2010-06-17
申请号：US12623034
申请日：2009-11-20
IPC分类号： G01V1/00
CPC分类号： G01V1/302 , G01V1/345 , G01V2210/48 , G01V2210/63 , G01V2210/641 , G01V2210/643 , G01V2210/66
摘要： A method of transforming geologic data relating to a subsurface region between a geophysical depth domain and a geologic age domain is disclosed. A set of topologically consistent surfaces is obtained that correspond to seismic data. The surfaces are enumerated in the depth domain. An age is assigned to each surface in the depth domain. The age corresponds to an estimated time of deposition of the respective surface. An age mapping volume is generated. An extent of the age domain is chosen. A depth mapping volume is generated. Both the age mapping volume and the depth mapping volume are used to transform geophysical, geologic, or engineering data or interpretations between the depth domain and the age domain and vice versa. The geophysical, geologic, or engineering data or interpretations transformed by at least one of the age mapping volume and the depth mapping volume are outputted.
摘要翻译： 公开了一种在地球物理深度域和地质年龄域之间转换与地下区域有关的地质数据的方法。 获得与地震数据相对应的一组拓扑一致的表面。 表面在深度域列举。 一个年龄分配给深度域中的每个表面。 该年龄对应于相应表面的估计沉积时间。 生成年龄映射卷。 选择年龄域的范围。 生成深度映射卷。 年龄映射卷和深度映射卷都用于在深度域和年龄域之间转换地球物理，地质或工程数据或解释，反之亦然。 输出由至少一个年龄映射卷和深度映射卷变换的地球物理，地质或工程数据或解释。
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2.发明授权Method for geophysical and geological interpretation of seismic volumes in the domains of depth, time, and age 有权深度，时间和年龄域的地震体积地球物理和地质解释方法公开(公告)号：US08213261B2
公开(公告)日：2012-07-03
申请号：US12881789
申请日：2010-09-14
IPC分类号： G01V1/30
CPC分类号： G01V1/32 , G01V2210/48 , G01V2210/63 , G01V2210/641 , G01V2210/643 , G01V2210/66
摘要： Method for transforming geologic data relating to a subsurface region between a geophysical depth domain and a geologic age domain. A set of topologically consistent surfaces (252a) is obtained that correspond to seismic data (252). The surfaces are enumerated in the depth domain. An age is assigned to each surface in the depth domain (255). The age corresponds to an estimated time of deposition of the respective surface. An age mapping volume is generated (256). An extent of the age domain is chosen. A depth mapping volume is generated (260). Both the age mapping volume and the depth mapping volume are used to transform geophysical, geologic, or engineering data or interpretations (258, 263) between the depth domain and the age domain (268) and vice versa (269). The geophysical, geologic, or engineering data or interpretations transformed by at least one of the age or depth mapping volume are outputted.
摘要翻译： 用于转换与地球物理深度域和地质年龄域之间的地下区域有关的地质数据的方法。 获得对应于地震数据（252）的一组拓扑一致的表面（252a）。 表面在深度域列举。 年龄分配给深度域中的每个表面（255）。 该年龄对应于相应表面的估计沉积时间。 生成年龄映射卷（256）。 选择年龄域的范围。 生成深度映射卷（260）。 年龄测绘卷和深度测绘卷都用于在深度域和年龄域（268）之间转换地球物理，地质或工程数据或解释（258,263），反之亦然（269）。 输出由至少一个年龄或深度映射卷变换的地球物理，地质或工程数据或解释。
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3.发明申请公开(公告)号：US20100161232A1
公开(公告)日：2010-06-24
申请号：US12623130
申请日：2009-11-20
CPC分类号： G01V1/302 , G01V1/345 , G01V2210/48 , G01V2210/63 , G01V2210/641 , G01V2210/643 , G01V2210/66
摘要： A computer-implemented method is provided for searching and analyzing a seismic data volume acquired in a seismic survey to determine potential for hydrocarbon accumulations in an associated subsurface region. Surfaces describing the seismic data volume are obtained. The surfaces are enumerated. At least one enumerated surface is selected. The at least one selected surface is augmented when the selected surface does not substantially cover an area associated with the seismic data volume. The augmenting is performed until all selected surfaces substantially cover the area. The at least one selected surface is displayed, with geologic or geophysical data associated therewith, for visual inspection or interpretation, or saving digital representations thereof to computer memory or data storage.
摘要翻译： 提供了一种计算机实现的方法，用于搜索和分析在地震勘测中获取的地震数据量，以确定相关地下区域中的碳氢化合物积聚的潜力。 获得描述地震数据体积的曲面。 表面被枚举。 选择至少一个枚举的表面。 当所选择的表面基本上不覆盖与地震数据量相关联的区域时，至少一个所选择的表面被增强。 执行增强，直到所有选定的表面基本上覆盖该区域。 显示至少一个所选择的表面，具有与其相关联的地质或地球物理数据，用于目视检查或解释，或将其数字表示保存到计算机存储器或数据存储器。
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4.发明申请Method For Geophysical and Geological Interpretation of Seismic Volumes In The Domains of Depth, Time, and Age 有权深度，时间和年龄域地震卷的地球物理和地质解释方法公开(公告)号：US20110002194A1
公开(公告)日：2011-01-06
申请号：US12881789
申请日：2010-09-14
IPC分类号： G01V1/00
CPC分类号： G01V1/32 , G01V2210/48 , G01V2210/63 , G01V2210/641 , G01V2210/643 , G01V2210/66
摘要： Method for transforming geologic data relating to a subsurface region between a geophysical depth domain and a geologic age domain. A set of topologically consistent surfaces (252a) is obtained that correspond to seismic data (252). The surfaces are enumerated in the depth domain. An age is assigned to each surface in the depth domain (255). The age corresponds to an estimated time of deposition of the respective surface. An age mapping volume is generated (256). An extent of the age domain is chosen. A depth mapping volume is generated (260). Both the age mapping volume and the depth mapping volume are used to transform geophysical, geologic, or engineering data or interpretations (258, 263) between the depth domain and the age domain (268) and vice versa (269). The geophysical, geologic, or engineering data or interpretations transformed by at least one of the age or depth mapping volume are outputted.
摘要翻译： 用于转换与地球物理深度域和地质年龄域之间的地下区域有关的地质数据的方法。 获得对应于地震数据（252）的一组拓扑一致的表面（252a）。 表面在深度域列举。 年龄分配给深度域中的每个表面（255）。 该年龄对应于相应表面的估计沉积时间。 生成年龄映射卷（256）。 选择年龄域的范围。 生成深度映射卷（260）。 年龄测绘卷和深度测绘卷都用于在深度域和年龄域（268）之间转换地球物理，地质或工程数据或解释（258,263），反之亦然（269）。 输出由至少一个年龄或深度映射卷变换的地球物理，地质或工程数据或解释。
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公开(公告)号：US09696442B2
公开(公告)日：2017-07-04
申请号：US14506178
申请日：2014-10-03
申请人： Weichang Li , Max Deffenbaugh , Dominique G. Gillard , Ganglin Chen , Xiaoxia Xu
发明人： Weichang Li , Max Deffenbaugh , Dominique G. Gillard , Ganglin Chen , Xiaoxia Xu
摘要： A hydrocarbon exploration method for determining subsurface properties from geophysical survey data. Rock physics trends are identified and for each trend a rock physics model is determined that relates the subsurface property to geophysical properties (103). The uncertainty in the rock physics trends is also estimated (104). A geophysical forward model is selected (105), and its uncertainty is estimated (106). These quantities are used in an optimization process (107) resulting in an estimate of the subsurface property and its uncertainty.
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6.发明申请Method for Estimating Subsurface Properties from Geophysical Survey Data Using Physics-Based Inversion 审中-公开使用基于物理的反演估算地球物理测量数据的地下特性的方法公开(公告)号：US20150120196A1
公开(公告)日：2015-04-30
申请号：US14506178
申请日：2014-10-03
申请人： Weichang Li , Max Deffenbaugh , Dominique G. Gillard , Ganglin Chen , Xiaoxia Xu
发明人： Weichang Li , Max Deffenbaugh , Dominique G. Gillard , Ganglin Chen , Xiaoxia Xu
摘要： A hydrocarbon exploration method for determining subsurface properties from geophysical survey data. Rock physics trends are identified and for each trend a rock physics model is determined that relates the subsurface property to geophysical properties (103). The uncertainty in the rock physics trends is also estimated (104). A geophysical forward model is selected (105), and its uncertainty is estimated (106). These quantities are used in an optimization process (107) resulting in an estimate of the subsurface property and its uncertainty.
摘要翻译： 一种用于从地球物理测量数据确定地下性质的烃探测方法。 确定岩石物理趋势，对于每种趋势，确定将地下性质与地球物理性质相关联的岩石物理模型（103）。 也估计了岩石物理趋势的不确定性（104）。 选择地球物理前向模型（105），估计其不确定度（106）。 这些数量用于优化过程（107），导致对地下属性及其不确定性的估计。
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7.发明授权Method for rapid fault interpretation of fault surfaces generated to fit three-dimensional seismic discontinuity data 有权用于快速故障解释的方法，用于生成适合三维地震不连续数据的故障表面公开(公告)号：US07330791B2
公开(公告)日：2008-02-12
申请号：US10527415
申请日：2003-09-17
CPC分类号： G01V1/32 , G01V1/301 , G01V2210/641
摘要： A method to extract fault surfaces from seismic data (1,3) is disclosed. The method comprises: (a) generating at least two fault sticks (5) from the same fault from at least two slices of the seismic data wherein each slice comprises at least one fault stick from the same fault, (b) constructing an initial three-dimensional fault surface (7) containing the fault sticks, and (c) reconstructing the initial fault surface (9) using a deformable surface model to fit discontinuity or coherency information in the seismic data in an iterative process. Techniques are disclosed for constructing the initial fault surface from interpreter-provided fault nodes, and for performing the deformable surface iteration by defining an energy function for the fault surface and then minimizing the surface energy.
摘要翻译： 公开了一种从地震数据中提取断层面的方法（1,3）。 该方法包括：（a）从地震数据的至少两个切片产生来自相同故障的至少两个断层（5），其中每个切片包括来自相同故障的至少一个断层，（b）构建初始三维 包含断层的三维断层面（7），（c）使用可变形表面模型重建初始断层面（9），以在迭代过程中对地震数据中的不连续性或一致性信息进行拟合。 公开了用于从解释器提供的故障节点构建初始故障表面的技术，并且通过为故障表面定义能量函数然后使表面能最小化来执行可变形表面迭代。
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公开(公告)号：US20110048731A1
公开(公告)日：2011-03-03
申请号：US12920013
申请日：2009-04-24
申请人： Matthias G. Imhof , Dominique G. Gillard , Stefan Hussenoeder , Dimitrov Pavel , Martin Terrell , Krishnan Kumaran , Fred Schroeder
发明人： Matthias G. Imhof , Dominique G. Gillard , Stefan Hussenoeder , Dimitrov Pavel , Martin Terrell , Krishnan Kumaran , Fred Schroeder
CPC分类号： G01V1/302 , G01V1/345 , G01V2210/48 , G01V2210/63 , G01V2210/641 , G01V2210/643 , G01V2210/66
摘要： Method for analysis of hydrocarbon potential of subterranean regions by generating surfaces or geobodies and analyzing them for hydrocarbon indications. Reflection-based surfaces may be automatically created in a topologically consistent manner where individual surfaces do not overlap themselves and sets of multiple surfaces are consistent with stratigraphic superposition principles. Initial surfaces are picked from the seismic data (41), then broken into smaller parts (“patches”) that are predominantly topologically consistent (42), whereupon neighboring patches are merged in a topologically consistent way (43) to form a set of surfaces that are extensive and consistent (“skeleton”). Surfaces or geobodies thus extracted may be automatically analyzed and rated (214) based on a selected measure (213) such as one or more direct hydrocarbon indications (“DHI”), e.g. AVO classification. Topological consistency for one or more surfaces may be defined as no self overlap plus local and global consistency among multiple surfaces (52).
摘要翻译： 通过产生表面或地球体分析地下区域的碳氢化合物潜力并分析烃类适应性的方法。 基于反射的表面可以以拓扑一致的方式自动创建，其中各个表面不重叠，多个表面的集合与地层叠加原理一致。 从地震数据（41）拾取初始表面，然后将其分解成主要是拓扑一致的较小部分（“补丁”）（42），于是以拓扑一致的方式（43）合并相邻的补丁以形成一组表面 这是广泛和一致的（“骨架”）。 可以基于所选择的措施（213）自动分析和评估如此提取的表面或地球物质，（214），例如一个或多个直接碳氢化合物指示（“DHI”），例如。 AVO分类。 一个或多个表面的拓扑一致性可以被定义为在多个表面之间没有自重叠加局部和全局一致性（52）。
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公开(公告)号：US06791900B2
公开(公告)日：2004-09-14
申请号：US10430173
申请日：2003-05-06
IPC分类号： G01V136
CPC分类号： G01V1/30
摘要： A method of calculating a throw volume corresponding to a seismic data volume. A range of time shifts and a search direction for the seismic data volume are selected. A data location separation and a vertical time window are also selected. A cross-correlation is calculated between data values corresponding to first and second data locations separated by the data location separation and symmetrically located in the search direction on each side of a target data location. The cross-correlation is calculated throughout the vertical time window for each time shift in the range of time shifts. The time shift corresponding to the maximum calculated cross-correlation is stored in the throw volume.
摘要翻译： 一种计算对应于地震数据量的投掷量的方法。 选择地震数据量的时间范围和搜索方向。 还选择数据位置分离和垂直时间窗口。 在对应于由数据位置分隔分隔的第一和第二数据位置的数据值之间计算互相关，并且在目标数据位置的每一侧对称地位于搜索方向。 在时间范围内的每个时间偏移的整个垂直时间窗口中计算互相关。 对应于最大计算的互相关的时移被存储在投掷量中。
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公开(公告)号：US20130151161A1
公开(公告)日：2013-06-13
申请号：US13757466
申请日：2013-02-01
申请人： Matthias G. Imhof , Dominique G. Gillard , Stefan Hussenoeder , Pavel Dimitrov , Martin J. Terrell , Krishnan Kumaran
发明人： Matthias G. Imhof , Dominique G. Gillard , Stefan Hussenoeder , Pavel Dimitrov , Martin J. Terrell , Krishnan Kumaran
CPC分类号： G01V1/003 , G01V1/301 , G01V2210/64 , G06F17/00
摘要： Method for analysis of hydrocarbon potential of subterranean regions by generating surfaces or geobodies and analyzing them for hydrocarbon indications. Reflection-based surfaces may be automatically created in a topologically consistent manner where individual surfaces do not overlap themselves and sets of multiple surfaces are consistent with stratigraphic superposition principles. Initial surfaces are picked from the seismic data (41), then broken into smaller parts (“patches”) that are predominantly topologically consistent (42), whereupon neighboring patches are merged in a topologically consistent way (43) to form a set of surfaces that are extensive and consistent (“skeleton”). Surfaces or geobodies thus extracted may be automatically analyzed and rated (214) based on a selected measure (213) such as AVO classification or one or more other direct hydrocarbon indicators (“DHI”). Topological consistency for one or more surfaces may be defined as no self overlap plus local and global consistency among multiple surfaces (52).
摘要翻译： 通过产生表面或地球体分析地下区域的碳氢化合物潜力并分析烃类适应性的方法。 基于反射的表面可以以拓扑一致的方式自动创建，其中各个表面不重叠，多个表面的集合与地层叠加原理一致。 从地震数据（41）拾取初始表面，然后将其分解成主要是拓扑一致的较小部分（“补丁”）（42），于是以拓扑一致的方式（43）合并相邻的补丁以形成一组表面 这是广泛和一致的（“骨架”）。 可以基于诸如AVO分类或一个或多个其他直接碳氢化合物指示器（“DHI”）的选定措施（213）自动分析和评估（214）所提取的表面或地球体。 一个或多个表面的拓扑一致性可以被定义为在多个表面之间没有自重叠加局部和全局一致性（52）。
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