首页> 外国专利> Generation of three dimensional fractal subsurface structure by Voronoi Tessellation and computation of gravity response of such fractal structure

Generation of three dimensional fractal subsurface structure by Voronoi Tessellation and computation of gravity response of such fractal structure

机译:Voronoi Tessellation生成三维分形地下结构以及这种分形结构的重力响应计算

摘要

Domain characterization generated by Voronoi tessellation, which is very close to realistic geology and computation of gravity response of such domain, has a three dimensional fractal basin structure, and is favorable for oil exploration. Interfaces or tessellating domains are represented by a set of parameters, which are referred as Voronoi centers. These parameters can be perturbed by any amount without getting into representational problems. To accomplish such representation Voronoi tessellation is used, which in two dimensional space involves enclosing every Voronoi center by a Voronoi polygon such that the common edge of adjacent polygons is a perpendicular bisector to the line joining the Voronoi centers on both the sides of that edge. Instead of using conventional Euclidian distances, the notion of Voronoi tessellation is generalized by using Lp distances, where p can hold any real value so that Voronoi domains are not necessarily polygonal. A desired fractal subsurface is generated using this approach that is quite close to the natural settings. Next, the gravity response due to this fractal subsurface structure is computed. A significant advantage is provided especially in geophysical inversion where initial model parameters are updated in each iteration, which can be done more easily and efficiently by Voronoi tessellation merely by changing Voronoi centers.
机译:Voronoi细分产生的区域特征非常接近于实际地质情况和该区域重力响应的计算,具有三维分形盆地结构,有利于石油勘探。接口或细分域由一组参数表示,这些参数称为Voronoi中心。这些参数可以不受任何干扰,而不会引起代表性问题。为了实现这种表示,使用了Voronoi细分,该细分在二维空间中包括用Voronoi多边形包围每个Voronoi中心,以使相邻多边形的公共边沿垂直于该边的两侧上连接Voronoi中心的线的等分线。通过使用L p 距离来概括Voronoi细分的概念,而不使用常规的Euclidian距离,其中p可以保留任何实数值,因此Voronoi域不一定是多边形。使用此方法生成的分形子表面非常接近自然设置。接下来,计算由于这种分形地下结构而引起的重力响应。特别是在地球物理反演方面提供了显着的优势,在这种情况下,每次迭代中都会更新初始模型参数,而仅通过更改Voronoi中心,通过Voronoi细分可以更轻松,更高效地完成。

著录项

  • 公开/公告号US7307629B2

    专利类型

  • 公开/公告日2007-12-11

    原文格式PDF

  • 申请/专利权人 RAVI SRIVASTAVA;V. DIMRI;

    申请/专利号US20040813649

  • 发明设计人 RAVI SRIVASTAVA;V. DIMRI;

    申请日2004-03-31

  • 分类号G06T17/20;G06T17/00;

  • 国家 US

  • 入库时间 2022-08-21 20:10:26

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