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METHOD OF 2-DIMENSIONAL SUBSURFACE GEOLOGICAL STRUCTURE ANALYSIS BY USING GRAVITY OR MAGNETIC SURVEY DATA

机译:利用重力或磁测量数据进行二维地下地质构造分析的方法

摘要

The present invention is the location of the expedition body of minerals, faults, discontinuities, oil, limestone cavities, too, groundwater, etc. pyegaeng present in underground by using the gravitational or magnetic sensing data obtained through various methods, such as the ground, aircraft, satellites 2 relates to a process to obtain a dimensionally, and more particularly, gravity or magnetic survey data traveling direction component existing Euler to identify the position of the sensing object by using the depth-direction component (Z-axis) to (X-axis) in - deconvolution to modify and improve the more accurately the position of the upper body expedition, and a method to obtain a two-dimensional position of the body to find the expedition objectively. ; Method using a gravity or magnetic survey data of the present invention to obtain the two-dimensional position of the upper body is expedition, ; (A) step of the gridded survey data to gridded at intervals along the measuring direction of the sensing data of measuring a gravity or magnetic force value of the predetermined interval; ; (B) a gridded sensing data of the sensing data to discern the direction and amount of change in the change amount separated in the vertical direction of the horizontal separation phase; ; (C) determining the size of the window and, by applying it to the equation (6) to a fixed position of the possible existence Euler finding expedition upper-stage deconvolution performed; comprises a, ; Wherein (c) by varying the size of the window in step Euler - and characterized in that the deconvolution performed several times, ; (D) determining the position (c) that is the highest frequency period by analyzing the presence of a possible location expedition body obtained through the steps to the position of the upper body expedition; and further comprising a. ; Gravity, magnetism, exploration data, groundwater, fault, joint, pyegaeng lattice, windows, Euler-deconvolution
机译:本发明是通过使用通过各种方法(例如地面)获得的重力或磁感应数据,在地下存在的矿物,断层,不连续性,油,石灰石空洞,地下水等pyegaeng探险队的所在地。在飞机上,卫星2涉及一种通过使用深度方向分量(Z轴)至(X -轴反褶积以更准确地修改和改善上身探险的位置,以及一种获取物体的二维位置以客观找到探险的方法。 ;使用本发明的重力或磁测量数据来获得上身的二维位置的方法是探险; (A)将网格化的调查数据沿着测量预定间隔的重力或磁力值的传感数据的测量方向以一定间隔网格化的步骤; ; (B)感测数据的网格化的感测数据,以辨别在水平分离相的垂直方向上分离的改变量的方向和改变量; ; (C)确定窗口的大小,并通过将其应用于方程式(6)的可能存在的固定位置,进行欧拉寻找远征上层反卷积;包括其中(c)通过在步骤Euler中改变窗口的大小,其特征在于,反卷积执行了几次, (D)通过分析通过到上身探险的位置的步骤获得的可能的位置探险体的存在,确定最高频率周期的位置(c);并且进一步包括;重力,磁性,勘探数据,地下水,断层,关节,pyegaeng晶格,窗,欧拉反褶积

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