首页> 外文期刊>International journal of remote sensing >Mapping alteration minerals at Malmbjerg molybdenum deposit, central East Greenland, by Kohonen self-organizing maps and matched filter analysis of HyMap data
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Mapping alteration minerals at Malmbjerg molybdenum deposit, central East Greenland, by Kohonen self-organizing maps and matched filter analysis of HyMap data

机译:通过Kohonen自组织图和HyMap数据的匹配过滤器分析,绘制东格陵兰中部Malmbjerg钼矿床的蚀变矿物

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摘要

The Malmbjerg molybdenum deposit in central East Greenland is a world-class porphyry molybdenum deposit. The porphyry molybdenum deposit occurs within a granite stock intruded into sedimentary rocks. The Malmbjerg molybdenum deposit is associated with a pronounced zone of hydrothermal alteration. The reflectance spectra of rock samples from the Malmbjerg alteration assemblage show absorption features of a number of minerals including topaz, jarosite, goethite, muscovite, phengite, epidote, chlorite and smectite. This study investigated the Malmbjerg alteration assemblage using airborne imaging spectrometer data recorded by the HyMap imaging system. The HyMap data were analysed using an unsupervised classification based on Kohonen self-organizing maps and partial spectral unmixing based on the matched filter algorithm. The mapping results show the spatial distribution of jarosite, goethite, phengite, epidote/chlorite, smectite, topaz and non-altered sediments. The remote-sensing mapping results bring new information for the alteration assemblage at Malmbjerg, especially for the occurrence and the spatial distribution of a phengite zone in the altered sediments overlying the molybdenum deposit and for the propylitic alteration zone. The study is an example of detailed characterization by imaging spectrometry of alteration assemblages associated with porphyry molybdenum deposits. This research also shows the potential of imaging spectrometry as a tool for geological mapping and exploration in the Arctic regions of East Greenland.
机译:东格陵兰中部的Malmbjerg钼矿床是世界一流的斑岩钼矿床。斑岩钼矿床发生在侵入沉积岩的花岗岩中。 Malmbjerg钼矿床与明显的热液蚀变带有关。来自Malmbjerg蚀变组合的岩石样品的反射光谱显示了许多矿物的吸收特征,包括黄玉,黄钾铁矾,针铁矿,白云母,变质铁矿,绿橄榄石,绿泥石和绿土。本研究使用由HyMap成像系统记录的机载成像光谱仪数据研究了Malmbjerg蚀变组合。使用基于Kohonen自组织图的无监督分类和基于匹配滤波器算法的部分光谱解混来分析HyMap数据。测绘结果显示了黄铁矿,针铁矿,锂铁矿,附子/绿泥石,蒙脱石,黄玉和未改变沉积物的空间分布。遥感测绘结果为马尔姆比尔格的蚀变组合提供了新的信息,特别是覆盖钼矿床的蚀变沉积物中的变质岩带的发生和空间分布,以及蚀变质带。该研究是通过成像光谱详细表征与斑岩钼矿床有关的蚀变组合的实例。这项研究还显示了成像光谱法作为东格陵兰岛北极地区地质绘图和勘探工具的潜力。

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  • 来源
    《International journal of remote sensing》 |2012年第4期|p.939-961|共23页
  • 作者

    ENTON BEDINP;

  • 作者单位

    Geological Survey of Denmark and Greenland (GEUS), Øster Voldgade 10, 1350 Copenhagen K, Denmark,Institute of Geography and Geology (IGG), Øster Voldgade 10, 1350 Copenhagen K,Denmark;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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