A combined Euler deconvolution and tilt angle method for interpretation of magnetic data in the South region

H. H. Nguyen, L. Dang, Vuong Van Vo
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引用次数: 1

Abstract

Introduction: The purpose of this paper is to determinate the position, depth, dip direction and dip angle the faults in the South region of Vietnam from the total magnetic intensity anomalies, that reduced to the magnetic pole (RTP). Methods: Based on the Oasis Montaj software, we proposed a new way to compute the positions and the depth to the top of the faults by combining the Tilt angle and the Euler deconvolution methods. In addition, the angle and direction of the dip of theses faults were also determined by considering maximum of the total horizontal derivative of the RTP upward continuation at the different height levels. Results: The results show that there are 12 faults along the longitudinal direction, latitudinal direction, Northwest — Southeast direction and Northeast — Southwest direction with the mazimum depth is about 3100 m and the dip angle changes in the range of 65-82◦. Results: These indicate that these methods are valuable tools for specifying the characteristics of geology, contribute to give and confirm the useful information on geological structure in the South region of Vietnam.  
南方地区磁资料的欧拉反褶积与倾角联合解释方法
摘要:本文的目的是利用还原到磁极(RTP)的总磁强异常来确定越南南部地区断层的位置、深度、走向和倾角。方法:基于Oasis Montaj软件,提出了一种结合Tilt角度和Euler反褶积方法计算断层顶部位置和深度的新方法。此外,通过考虑RTP在不同高度水平向上延伸的总水平导数的最大值,确定了这些断裂的倾角角度和方向。结果:研究结果表明,断层沿纵向、纬向、西北—东南方向和东北—西南方向分布有12条断层,最大深度约为3100 m,倾角变化范围为65 ~ 82◦。结果:这些方法是明确越南南部地区地质特征的有价值的工具,有助于提供和确认越南南部地区地质构造的有用信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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