首页> 外国专利> 3D MAGNETIC INVERSION METHOD BASED ON THE ASSEMBLAGE OF 2D FORWARD MODELING AND INVERSION AS A TECHNIQUE TO REFLECT THE A-PRIORI INFORMATION

3D MAGNETIC INVERSION METHOD BASED ON THE ASSEMBLAGE OF 2D FORWARD MODELING AND INVERSION AS A TECHNIQUE TO REFLECT THE A-PRIORI INFORMATION

机译:基于2D正演与反演组合的3D磁反演方法作为一种反映先验信息的技术

摘要

The present invention proposes a method for reflecting three-dimensional (3D) advance information and, particularly, a 3D magnetic inversion method for reflecting advance information using two-dimensional (2D) forward modeling and 2D inversion, which is capable of forming a 3D advance information model and a 3D initial magnetic susceptibility model based on a combination of 2D forward modeling and 2D inversion and performing 3D magnetic inversion based on the models. The proposed method of the present invention comprises the steps of: selecting a region of interest to perform 3D magnetic inversion on a magnetic anomaly map for a research area and separating 2D measuring lines in the selected region of interest; forming a combination of 2D measuring lines using data on the 2D measuring lines separated in the region of interest, respectively performing 2D forward modeling and 2D inversion for 2D measuring lines included in advance information, respectively generating a set of 2D weighting function sections and a set of 2D magnetic susceptibility sections for the 2D measuring line data, and respectively a 3D advance information model and a 3D initial model using the set of 2D weighting function sections and the set of 2D magnetic susceptibility sections; progressing 3D magnetic inversion for the region of interest using the 3D advance information model and the 3D initial model; and displaying a magnetic susceptibility cube for the region of interest. Thus, the method for reflecting advance information using 2D forward modeling and 2D inversion of the present invention is a practical technique capable of successively lessening non-uniqueness of 3D magnetic inversion and drawing geologically meaningful, reasonable inversion results. [Reference numerals] (S11) Input a magnetic anomaly map for a research area; (S13) Display a region of interest on the magnetic anomaly map; (S15) Display 2D measuring lines in the region of interest; (S21-1) 2D forward modeling; (S21-2) 2D inversion; (S23-1) Generate 2D weighting function sections; (S23-2) Generate 2D magnetic susceptibility sections; (S25-1,S25-2) Input all the advance information; (S27-1) Generate a 3D advance information model; (S27-2) Generate a 3D initial model; (S30) 3D inversion; (S40) Analyze a magnetic susceptibility cube
机译:本发明提出了一种用于反映三维(3D)超前信息的方法,特别是一种用于利用二维(2D)正向建模和2D反演来反映超前信息的3D磁反演方法,其能够形成3D超前。信息模型和基于2D正演建模和2D反演的3D初始磁化率模型,并基于这些模型执行3D磁反演。本发明提出的方法包括以下步骤:选择感兴趣区域以在研究区域的磁异常图上执行3D磁性反演,并在选定的感兴趣区域中分离2D测量线;使用在感兴趣区域中分离的2D测量线上的数据形成2D测量线的组合,分别对预先信息中包含的2D测量线执行2D正向建模和2D反演,分别生成2D加权函数部分集和使用该组2D加权函数部分和该组2D磁化率部分,针对2D测量线数据的2D磁化率部分,以及3D超前信息模型和3D初始模型;使用3D超前信息模型和3D初始模型对感兴趣区域进行3D磁反演;并显示感兴趣区域的磁化率立方体。因此,本发明的使用2D正演建模和2D反演来反映超前信息的方法是一种实用技术,能够连续减轻3D磁反演的不唯一性并得出地质上有意义的合理反演结果。 [附图标记](S11)输入研究区域的磁异常图。 (S13)在磁异常图上显示关注区域; (S15)在关注区域显示二维测量线; (S21-1)2D正向建模; (S21-2)2D反演; (S23-1)生成2D加权函数区间; (S23-2)生成二维磁化率截面; (S25-1,S25-2)输入所有提前信息; (S27-1)生成3D超前信息模型; (S27-2)生成3D初始模型; (S30)3D反转; (S40)分析磁化率立方体

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