南非吉雅尼绿岩带ASTER数据的金相关蚀变矿物及线性构造填图

IF 0.3 Q4 REMOTE SENSING South African Journal of Geomatics Pub Date : 2022-09-07 DOI:10.4314/sajg.v9i2.17
Nndanduleni Muavhi, Mbofholowo Emmanuel Mavhungu
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引用次数: 5

摘要

本文重点研究了Giyani绿岩带(GGB)蚀变矿物和与金矿化相关的线性结构图。使用图像提取的端元光谱,将光谱信息发散(SID)和线性光谱未混合(LSU)分类算法应用于ASTER数据,这些端元光谱与GGB中与金矿化相关的主要蚀变矿物(黑云母和方解石)的光谱轮廓相匹配。定向卷积滤波器也应用于ASTER数据,以提取可能与金矿化有关的结构线理。此外,对GGB中已知的金矿进行了Fry分析,以确定金矿化发生的主要分布模式。LSU和SID结果显示,几个像素被归类为与已知金矿点相对应的蚀变矿物。SID结果还显示,矿物重叠在片麻岩中,这是研究区罕见的金矿化宿主。另一方面,LSU结果显示,方解石和黑云母的丰度很高,通常局限于镁铁质-超镁铁质绿岩中,这些岩石被假设为GGB中金矿化流体的来源。总的来说,LSU显示了不同的广泛区域,这些区域被归类为蚀变矿物,与之前报道的含有这些蚀变矿物的已知金矿相对应。定向卷积滤波器能够提取主要为NE-SW方向的线性结构,包括与GGB中金矿化相关的主要剪切带。Fry分析揭示了三种主要的金矿化分布模式:N-S、NE-SW、ENE-WSW。这些模式对应于GGB先前结构研究中报告的与金矿化相关的主要线性构造。
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Mapping of gold-related alteration minerals and linear structures using ASTER data in the Giyani Greenstone Belt, South Africa
This paper focuses on the mapping of alteration minerals and linear structures associated with gold mineralization in the Giyani Greenstone Belt (GGB). Spectral Information Divergence (SID) and Linear Spectral Unmixing (LSU) classification algorithms were applied to the ASTER data using image extracted endmember spectra which match the spectral profiles of predominant alteration minerals (biotite and calcite) related to gold mineralization in the GGB. Directional convolution filters were also applied to the ASTER data to extract structural lineaments that may be related to gold mineralization. In addition, Fry analysis of known gold occurrences in the GGB was conducted to determine the major distribution patterns along which gold mineralization have occurred. LSU and SID results show several pixels classified as alteration minerals corresponding to known gold occurrences. SID results also show minerals overlapping into the gneissic rock, which is a rare host of gold mineralization in the study area. On the other hand, LSU results show high abundances of calcite and biotite generally confined within the mafic-ultramafic greenstone rocks, which have been hypothesized as the source of gold-mineralized fluids in the GGB. In general, LSU show distinct broad regions classified as alteration minerals corresponding to known gold occurrences that have been previously reported to host these alteration minerals. Directional convolution filters enabled the extraction of predominately NE-SW oriented linear structures, including the major shear zone which is associated with gold mineralization in the GGB. Fry analysis revealed three major distribution patterns: N-S, NE-SW, ENE-WSW along which gold mineralization have occurred. These patterns correspond to major lineaments associated with gold mineralization reported in the previous structural studies of the GGB.
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