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1. 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。

2. 发明授权

US10114134B2 Systems and methods for generating a geological model honoring horizons and faults 有权
公开(公告)号：US10114134B2
公开(公告)日：2018-10-30
申请号：US13458264
申请日：2012-04-27
申请人： Wan-Chiu Li , Laurent Deny , Olivier Grosse , Jean-Claude Dulac
发明人： Wan-Chiu Li , Laurent Deny , Olivier Grosse , Jean-Claude Dulac
IPC分类号： G06G7/48 , G01V1/32 , G01V99/00
摘要： A system and method for modeling a subsurface structure. Data representing a configuration of faults, horizons, and/or unconformities may be transformed to a depositional model comprising cells representing an estimated configuration of subsurface structure at a depositional time period when the subsurface structure was formed. Groups of cells in the depositional model may be divided into sub-meshes using iso-surfaces, where one set of iso-surfaces may represent the horizons at the depositional time period. The sub-meshes may be divided into one or more parts using the transformed geological data representing an estimated depositional configuration of the faults. For each group of cells in each sub-mesh part, the group of cells in the sub-mesh part may be represented by a single polyhedron. The polyhedrons may be transformed to generate a current model to represent the current configuration of the faults and horizons using transformed polyhedrons.

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