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Detection of regions of structural complexity within aeromagnetic data using image analysis

机译:使用图像分析检测航空数据中结构复杂性的区域

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Mineral exploration requires selecting grounds where exploration is to be conducted. Ground selection and mineralisation targeting processes require identification of areas with specific geological settings. For exploration of Archaean lode gold deposits, crustal breaks are used as conduits for mineralising fluids and their structural associations such as crossings, junctions, and changes of orientations are closely associated with mineralisation. Aeromagnetic data represent magnetic response variations from the Earth's crust, and discontinuities in these data reveal crustal breaks, along with lithological boundaries and dykes that are important for understanding the local geology. This paper presents on-going image analysis research that aims to detect such characteristics within aeromagnetic data automatically, in order to provide an efficient and non-subjective analysis for gold prospectivity mapping. The proposed method automatically highlights the regions of high structural complexity within regional datasets. It firstly finds regions of magnetic discontinuity using a combination of texture analysis and bilateral symmetric feature detection, where line-like features representing high local magnetic variations are identified. Using skeletal structures of the identified regions of discontinuity it analyses structure associations to locate their intersections as well as to find orientation variations of neighbouring structures. Finally, by applying an accumulative Gaussian weighting, it generates heat maps that highlight the areas that are perceived to be prospective. A preliminary experiment was conducted using aeromagnetic data from the Yilgarn Craton in Western Australia and the regions selected by the proposed system are highly correlated with the known gold deposits in the area.
机译:矿物勘探需要选择进行勘探的场所。地面选择和矿化目标确定过程需要识别具有特定地质环境的区域。为了勘探古生的金矿床,地壳破裂被用作矿化流体的管道,并且它们的构造联系(例如交叉,交汇和方向变化)与矿化密切相关。航磁数据代表了地壳的磁响应变化,这些数据的不连续性揭示了地壳破裂以及对理解当地地质状况至关重要的岩性边界和堤坝。本文介绍了正在进行的图像分析研究,旨在自动检测航空磁数据中的此类特征,以便为金前景图提供有效且非主观的分析。所提出的方法自动突出显示区域数据集中结构高度复杂的区域。它首先结合纹理分析和双边对称特征检测找到磁不连续区域,在其中识别出代表高局部磁变化的线状特征。使用已识别的不连续区域的骨骼结构,它可以分析结构关联以找到它们的交点,并找到相邻结构的方向变化。最后,通过应用累积的高斯加权,它会生成热图,突出显示被认为是潜在区域的区域。利用来自西澳大利亚的伊尔加恩·克拉顿(Yilgarn Craton)的航空磁数据进行了初步实验,该系统选择的区域与该地区已知的金矿床高度相关。

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