高分辨率航磁测量下海槽线与矿化的圈定:以abakikili 303薄片为例

C. Okpoli
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引用次数: 6

摘要

利用Abakiliki (303 SW薄片)的高分辨率航磁数据集对尼日利亚Lower Benue海槽的部分地下岩石构造特征进行了表征。为了促进国家的经济,这项研究对于绘制和划定油气勘探区域是必要的。对航磁数据进行了多种形式的过滤、还原和增强技术,以进行定性和定量解释。赤道总磁场强度还原(RTE-TMI)结果显示,地下岩石的磁场强度在34.14 ~ 61.40nT之间。该范围内的岩石主要为Asu河组页岩和灰岩、Awgu页岩、Eze-AKu页岩和Nkporo页岩。RTE-TMI数据向上延续至500m、1 km、2 km、3 km、7 km和10 km,揭示了这些岩石和构造随着测量深度的延续而变薄的区域趋势。垂直二次导数(SVD)、倾斜导数(TDR)和解析信号(AS)显示出3条主要断层;F1-F11、F2F12和F3-F13分别位于NE-SW、ENE-WSW和NW-SE方向。径向平均功率谱(RAPS)和欧拉反褶积显示,较浅源和较深源的磁源至顶深度分别为27m和2.64km。这项研究证明了航磁方法的有效性,其改进的技术可以作为区域岩性和结构测绘的工具,这些区域可能含有重要的矿物和/或有助于油气聚集及其可能的深度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
DELINEATION OF HIGH-RESOLUTION AEROMAGNETIC SURVEY OF LOWER BENUE TROUGH FOR LINEAMENTS AND MINERALIZATION: CASE STUDY OF ABAKIKILI SHEET 303
High resolution aeromagnetic dataset of Abakiliki (sheet 303 SW) was used for the characterization of the subsurface lithostructural features in part of the Lower Benue Trough, Nigeria. This study was necessitated for mapping and delineating hydrocarbon prospecting zones, in order to boost the Nation’s economy. The aeromagnetic data were subjected to several forms of filtering, reductions, and enhancement techniques for both qualitative and quantitative interpretations. The result of the reduction to equatortotal magnetic intensity (RTE-TMI) revealed the magnetic intensity of subsurface rocks ranging from 34.14nT to 61.40nT. These range of magnetic intensity values characterized the rocks in the area as shale and Limestone within the Asu River Group, Awgu shale, Eze-AKu shale and Nkporo shale. The upward continued RTE-TMI data to 500m, 1 km, 2 km, 3 km, 7 km and 10 km revealed regional trends of these rocks and structure thin –out with measure depth continuation. The second vertical derivative (SVD), Tilt-angle derivative (TDR) and Analytical signal (AS) revealed three (3) major faults; F1-F11, F2F12 and F3-F13 in NE-SW, ENE-WSW and NW-SE directions respectively. The depth to top of magnetic source were revealed by the radially averaged power spectrum (RAPS) and Euler deconvolution as 27m and 2.64km for shallower and deeper sources respectively. This study has demonstrated the efficiency of aeromagnetic methods, with their improved techniques as tools for regional mapping of lithologies and structures that may host important minerals and/or aid hydrocarbon accumulation and their probable depths.
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