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21. 发明授权

US10310137B1 Systems and methods for building axes, co-axes and paleo-geographic coordinates related to a stratified geological volume 有权
公开(公告)号：US10310137B1
公开(公告)日：2019-06-04
申请号：US15205281
申请日：2016-07-08
申请人： Paradigm Sciences Ltd. , Jean-Laurent Mallet
发明人： Jean-Laurent Mallet
IPC分类号： G01V1/32 , G06F17/16 , G01V99/00 , G06T17/05
摘要： A method and system for modeling a subsurface structure at a time when the structure was originally formed. A first model having non-planar horizons representing a current subsurface structure may be used to calculate a vector field based on the non-planar geometry of the horizons of the model. The vector field may be non-uniform or uniform. Geographic coordinates of the first model may be transformed to paleo-geographic coordinates of a model representing the subsurface structure in the past, where the non-planar horizons in the first model are transformed to planar horizons in the second model. A set of points describing one or more fractures in the subsurface structure may be used to calculate a tuning parameter to correct a first set of paleo-geographic coordinates. A second set of coordinates representing an improved prediction at a time period when the subsurface structure was originally formed may be generated.

22. 发明授权

US10222508B2 Systems and methods to build sedimentary attributes 有权
公开(公告)号：US10222508B2
公开(公告)日：2019-03-05
申请号：US15812604
申请日：2017-11-14
申请人： PARADIGM SCIENCES LTD. , Jean-Laurent Mallet
发明人： Jean-Laurent Mallet
IPC分类号： G01V99/00
摘要： A method and system for computing and visualizing sedimentary attributes may include receiving, by a processor, paleo-geographic coordinates representing predicted approximate positions of particles of sediment deposited at a time period when a layer was originally formed. The processor may numerically compute or determine a sedimentation rate that varies laterally along the layer. The processor may determine a sedimentary attribute based on the lateral variation of the sedimentation rate along the layer with respect to the paleo-geographic coordinates. A monitor or display may display the sedimentary attribute of the layer in the present-day geological space.

23. 发明授权

US09728003B1 Systems and methods for coordinated editing of seismic data in dual model 有权
公开(公告)号：US09728003B1
公开(公告)日：2017-08-08
申请号：US15166438
申请日：2016-05-27
申请人： PARADIGM SCIENCES LTD. , Jean-Laurent Mallet
发明人： Jean-Laurent Mallet , Jean-Claude Dulac , Emmanuel Labrunye , Christophe Winkler , Laurent Deny
IPC分类号： G06T17/05 , G06T19/20 , G06T3/20 , G01V1/30
CPC分类号： G06T17/05 , G01V1/302 , G01V99/005 , G01V2210/64 , G01V2210/66 , G06T3/20 , G06T19/20 , G06T2200/04 , G06T2207/30181 , G06T2219/2021
摘要： A system and method may model physical geological structures. Seismic and geologic data may be accepted. A three-dimensional (3D) transformation may be generated between a 3D present day model having points representing present locations of the physical geological structures and a 3D past depositional model having points representing locations where the physical geological structures were originally deposited. An indication may be accepted to locally change the 3D transformation for a subset of sampling points in a first model of the models. The 3D transformation may be locally changed to fit the updated subset of sampling points. A locally altered or updated version of the first model and, e.g., second model, may be displayed where local changes to the first model are defined by the locally changed 3D transformation. The transformation may also be used to extract geobodies in the past depositional model.

24. 发明授权

US08635052B1 Method and appartus for transforming a stratigraphic grid 有权
标题翻译：用于转换地层格栅的方法和方法
公开(公告)号：US08635052B1
公开(公告)日：2014-01-21
申请号：US12795494
申请日：2010-06-07
申请人： Jean-Laurent Mallet , Wan-Chiu Li , Jean-Claude Dulac
发明人： Jean-Laurent Mallet , Wan-Chiu Li , Jean-Claude Dulac
IPC分类号： G06G7/48
CPC分类号： G06T17/05 , G06T17/20
摘要： A method of transforming an input stratigraphic grid SGrid which represents a region including one or more geological discontinuities is now disclosed. At least one target cell that is local to one or more geological discontinuities is transformed by displacing at least one target vertex of the target cell of the input SGrid in a selected direction that: i) is selected to approximate a local tangent of the reference horizon; and ii) is oriented from the target vertex to a representative manifold representing one of the geological discontinuities and/or an intersection between two or more of the geological discontinuities. A magnitude of a displacement by which the target vertex is moved is determined according to a non-Euclidian distance between the target vertex of the target cell of the input SGrid and the representative manifold.
摘要翻译：现在公开了一种转换表示包括一个或多个地质不连续区域的输入地层格栅SGrid的方法。通过在所选择的方向上移位输入的SGrid的目标单元的至少一个目标顶点来转换对一个或多个地质不连续性局部的至少一个目标单元，其中：i）被选择为近似参考水平面的局部切线 ; 并且ii）从目标顶点定向到表示地质不连续性之一和/或两个或更多个地质不连续点之间的交叉点的代表性歧管。根据输入的SGrid的目标单元的目标顶点和代表歧管之间的非欧几里德距离来确定移动目标顶点的位移的大小。

25. 发明授权

US08150663B2 Partitioning algorithm for building a stratigraphic grid 有权
标题翻译：用于构建地层网格的分区算法
公开(公告)号：US08150663B2
公开(公告)日：2012-04-03
申请号：US11729980
申请日：2007-03-30
申请人： Jean-Laurent Mallet
发明人： Jean-Laurent Mallet
IPC分类号： G06G7/48
CPC分类号： G01V11/00 , G01V2210/66 , G06F17/5004 , G06F17/5009
摘要： Embodiments of the invention provide a system and method for partitioning data for modelling a geological structure including laterally partitioning the data into multiple columns, where each column may be substantially laterally centered about a dual fiber and vertically partitioning each column at each of multiple intersection points of multiple surfaces and the dual fiber about which the column may be substantially laterally centered.
摘要翻译：本发明的实施例提供了一种用于对用于对地质结构进行建模的数据分区的系统和方法，包括将数据横向分割成多个列，其中每个列可以基本上横向地围绕双纤维居中并且在每个多个交点多个表面和双纤维，柱可以围绕该双纤维基本上横向居中。

26. 发明授权

US07561992B2 Process, device and package for stochastic simulation of ancient riverbeds or ancient geological structures 有权
标题翻译：古代河床或古代地质构造随机模拟的过程，装置和包装
公开(公告)号：US07561992B2
公开(公告)日：2009-07-14
申请号：US11100467
申请日：2005-04-07
申请人： Bruno Leflon , Emmanuel Gringarten , Jean-Laurent Mallet
发明人： Bruno Leflon , Emmanuel Gringarten , Jean-Laurent Mallet
IPC分类号： G06F17/10 , G06G7/48
CPC分类号： G01V11/00 , G01V2210/665
摘要： A process for stochastic simulation of ancient riverbeds or ancient geological structures includes the following stages: (a) parameterize the geological reference horizon by linking to it a two-dimensional parametric system of paleogeographic coordinates; (b) construct a modeling function, the isovalue curves of which are approximately parallel to the general direction of the ancient riverbed to be simulated; (c) use the absolute value of the modeling function of the general direction of the ancient riverbed to be located in order to define a topographic function of the pseudo-valley; (d) transform the topographic function of the pseudo-valley by using a transfer function to determine the thicknesses, dimensions and characteristics of the ancient riverbed to be located and/or the ancient geological structures associated with this ancient riverbed.
摘要翻译：古河床或古代地质构造随机模拟的过程包括以下几个阶段：（a）通过连接地质参考地图参数化地质坐标二维参数系统; （b）构造建模函数，其等值曲线大致平行于待仿真的古河床的大致方向; （c）使用古河床总方向的建模函数的绝对值来定义伪谷的地形函数; （d）通过使用传递函数来转换伪谷的地形函数，以确定与这个古老河床相关联的古老河床的厚度，尺寸和特征和/或古代地质结构。

27. 发明申请

US20080021684A1 Method For Building A Three Dimensional Cellular Partition Of A Geological Domain 有权
标题翻译：建立地质域三维细胞分区的方法
公开(公告)号：US20080021684A1
公开(公告)日：2008-01-24
申请号：US11628559
申请日：2004-06-02
申请人： Jean-Claude Dulac , Jean-Laurent Mallet
发明人： Jean-Claude Dulac , Jean-Laurent Mallet
IPC分类号： G06G7/50
CPC分类号： G01V11/00
摘要： The invention concerns a method for building a three-dimensional (3D) cellular partition covering a 3D geological domain by defining the cells of the partition, characterized in that said method comprises the following steps A “3D screen construction step” for constructing a 3D screen which is a 3D elementary partition covering the geological domain, said 3D screen being composed of a plurality of voxels (Vi) which are elementary volume elements, A “voxel painting step” for associating a cell identifier (Cell-id) to each voxel, A “cell definition step” for defining the cells of the geological domain, each cell of the geological domain being defined as the subset of voxels of the 3D screen associated to the same cell identifier, thereby allowing the definition of the cells of the geological domain without having to code the geometry and/or topology of said cells in said geological volume. The invention further provides a “parametric” method and a “cookiecutter” method using such method for building a 3D cellular partition.
摘要翻译：本发明涉及通过定义分区的单元来构建覆盖3D地质域的三维（3D）蜂窝分区的方法，其特征在于所述方法包括以下步骤：用于构建3D屏幕的“3D屏幕构造步骤” 所述3D屏幕由作为基本体元件的多个体素（Vi）组成; A“体素绘画步骤”，用于将单元标识符（Cell-id）与每个体素相关联，用于定义地质域的单元的“单元定义步骤”，地质域的每个单元被定义为与相同的单元标识符相关联的3D屏幕的体素的子集，由此允许对地质域的单元格的定义而不必对所述地质体积中的所述细胞的几何和/或拓扑进行编码。本发明还提供了一种使用这种用于构建3D蜂窝分区的方法的“参数”方法和“烹饪器”方法。

28. 发明授权

US06820043B2 Modeling continuous properties on discontinuous surfaces 失效
标题翻译：在不连续表面上建模连续性质
公开(公告)号：US06820043B2
公开(公告)日：2004-11-16
申请号：US09927417
申请日：2001-08-09
申请人： Jean-Laurent Mallet , Richard Cognot , T. Ait Ettajer
发明人： Jean-Laurent Mallet , Richard Cognot , T. Ait Ettajer
IPC分类号： G06F1710
CPC分类号： G06F17/5018
摘要： A method of establishing continuity of a property which is interpolated over a surface defined by at least two primary nodes. The method includes identifying first and second portions of a boundary which defines a discontinuity in the surface. The method further includes defining the first and second portions of the boundary by at least one secondary node on each portion, and interpolating the property from a first primary node to a second primary node by utilizing the secondary nodes. When the property is characterized by determined values at primary nodes on the surface, the continuity of the property can be established as substantially the same value of the property at the selected secondary nodes. When the surface is characterized by a given gradient at each of the secondary nodes, the continuity of the property can be established as substantially the same gradient at the selected secondary nodes.
摘要翻译：一种建立在由至少两个主节点限定的表面上插值的属性的连续性的方法。该方法包括识别限定表面中的不连续性的边界的第一和第二部分。该方法还包括通过每个部分上的至少一个辅助节点来界定边界的第一和第二部分，以及通过利用次要节点将属性从第一主节点内插到第二主节点。当属性在表面上的主节点上由确定的值表征时，可以将属性的连续性建立为在所选择的次节点处的基本相同的属性值。当表面在每个次级节点处以给定的梯度表征时，可以将所述属性的连续性建立为在所选次级节点处基本上相同的梯度。

29. 发明授权

US10338252B1 Systems and processes for building multiple equiprobable coherent geometrical models of the subsurface 有权
公开(公告)号：US10338252B1
公开(公告)日：2019-07-02
申请号：US15203633
申请日：2016-07-06
申请人： PARADIGM SCIENCES LTD. , Jean-Laurent Mallet
发明人： Jean-Laurent Mallet , Anne-Laure Tertois
IPC分类号： G01V1/34 , G01V1/36 , G01V1/28 , G06T19/20 , G01V1/30 , G06T17/00 , G01V99/00
摘要： A method, apparatus and system for, in a computing system, perturbing an initial three-dimensional (3D) geological model using a 3D vector field. A coherent 3D vector field including 3D vectors may be generated where each 3D vector of the 3D vector field is associated with a node of the initial 3D geological model and has a magnitude within a range of uncertainty of the node of the initial 3D geological model associated therewith. The coherent 3D vector field may be applied to the initial 3D geological model associated therewith to generate an perturbed 3D model. The perturbed 3D model may differ from the initial 3D geological model by a displacement defined by the 3D vector field associated with nodes having uncertain values. The perturbed 3D model may be displayed.

30. 发明授权

US10331817B1 Systems and methods for modeling faults in the subsurface 有权
公开(公告)号：US10331817B1
公开(公告)日：2019-06-25
申请号：US15299566
申请日：2016-10-21
申请人： PARADIGM SCIENCES LTD. , Jean-Laurent Mallet
发明人： Anne-Laure Tertois , Jean-Laurent Mallet , Laurent Deny , Jean-Claude Dulac
IPC分类号： G06F17/10 , G06F17/50 , G06F17/16
摘要： A method, apparatus and system for modeling a fault surface in a subsurface region. A direction may be determined in which a first portion of the subsurface region being on one side of the fault surface has moved relative to a second portion of the subsurface region being on the other side of the fault surface. A model of the fault surface may be generated having substantially no protrusions in the determined direction. A visualization of the model of the generated fault surface may be displayed.

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