发明名称 Method of analyzing 3D geological structure using structure index
摘要 A method of analyzing a 3D geological structure using a structure index. The method includes the steps of estimating physical property values on common coordinates to calculate two or more physical property models on the same 3D grid (L×M×N); normalizing the physical property models, thus obtaining normalized physical property models which are then represented in a scatter plot of physical properties; converting distribution positions of the normalized physical property models on the scatter plot of physical properties into type angle (TA) and into type intensity (TI); determining a minimum of TI values, which classifies two or more classes on a scatter plot of the TA and TI values, to be a threshold; and analyzing the 3D geological structure based on a local extreme point and/or points in the scatter plot for the TA and TI using the threshold.
申请公布号 US9563602(B2) 申请公布日期 2017.02.07
申请号 US201213618105 申请日期 2012.09.14
申请人 KOREA INSTITUTE OF GEOSCIENCE AND MINERAL RESOURCES 发明人 Park Gyesoon;Heo Chul-Ho
分类号 G06F17/10;G01V11/00;G01V99/00 主分类号 G06F17/10
代理机构 Fredrikson & Byron, P.A. 代理人 Fredrikson & Byron, P.A.
主权项 1. A method of analyzing a three-dimensional (3D) geological structure, comprising: estimating a density value and a resistivity value on common coordinates L, M, and N to calculate a density model Ddata (L,M,N) and a resistivity model Rdata (L,M,N) on a same 3D grid (L×M×N), thus obtaining physical property models; normalizing the physical property models, thus obtaining normalized physical property models NDdata (L,M,N) and NRdata (L,M,N) which are then represented in a scatter plot of physical properties; converting distribution positions of the NDdata (L,M,N) and NRdata (L,M,N) on the scatter plot of physical properties into type angle (TA) using a four-quadrant inverse tangent and into type intensity (TI) using a distance from an origin; determining a minimum of TI values, which classifies two or more classes on a scatter plot of the TA and TI values, to be a threshold; and analyzing the 3D geological structure based on a local extreme point and/or points in the scatter plot for the TA and TI using the threshold, wherein analyzing the 3D geological structure is performed by determining a rock type, and a structure depending on physical properties and geological positions of the classes.
地址 Daejeon KR