...
首页> 外文期刊>International Journal of Geosciences >Inferring the Subsurface Basement Depth and the Contact Locations from Aeromagnetic Data over Loum-Minta Area (Centre-East Cameroon)
【24h】

Inferring the Subsurface Basement Depth and the Contact Locations from Aeromagnetic Data over Loum-Minta Area (Centre-East Cameroon)

机译:从卢姆·明塔地区(喀麦隆中东部)的航空磁数据推断地下地下室的深度和接触位置

获取原文
   

获取外文期刊封面封底 >>

       

摘要

The present study aims to estimate the basement depth and contact locations, deduced from the available aeromagnetic data. The total intensity aeromagnetic (TMI) map was fi rst corrected by the application of the reduction to equator technique. Different edge detection processes, for example, tilt angle derivative (TDR) and its total horizontal derivative (HD_TDR) as well as 3D-Euler deconvolution can determine the edges of these sources. These techniques were carried out on the aeromagnetic data of Minta region (the study area). A correlation was noticed between these techniques indicating that both of them can be attributed in delineating the general structural framework of the area. The aeromagnetic data analysis enables to highlight many deeply-seated structural features trending in the E-W, ENE-WSW and NE-SW directions in this region. The E-W trend is more strongly developed than the other identified trends. Moreover that, two depth methods were applied: analytic signal (AS) and source parameter imaging (SPI). They r efl ected similar results for estimating the basement depths. From both of them the depth ranges from 150 to 2800 m. Five methods (TDR, HD_TDR, 3D-Euler deconvolution, AS and SPI) for locating magnetic sources indicated that the depth of the basement rocks range d between 150 and 3000 m as the average range. Also, the comparative study among the 2D magnetic modeling was established by one profile constructing.
机译:本研究的目的是估计地下室的深度和接触位置,从可用的航磁数据推导出来。总强度航空电磁(TMI)图首先通过将赤道技术应用于赤道技术进行了校正。不同的边缘检测过程(例如,倾斜角导数(TDR)及其总水平导数(HD_TDR)以及3D-Euler反卷积)可以确定这些源的边缘。这些技术是对Minta地区(研究区域)的航空磁数据进行的。注意到这些技术之间的相关性,表明它们两者都可以归因于描绘该地区的总体结构框架。航磁数据分析可以突出显示该区域在E-W,ENE-WSW和NE-SW方向上趋势发展的许多深层次结构特征。与其他已确定的趋势相比,E-W趋势更加强大。此外,应用了两种深度方法:分析信号(AS)和源参数成像(SPI)。他们得出了相似的结果来估计地下室的深度。两者的深度范围均为150至2800 m。定位磁源的五种方法(TDR,HD_TDR,3D-Euler反卷积,AS和SPI)表明,基底岩石的深度d的平均范围为150至3000 m。此外,通过一种轮廓构造建立了二维磁性建模之间的比较研究。

著录项

相似文献

  • 外文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号