Abstract

Hydrothermal alteration minerals are an effective prospecting indicator. Advanced spaceborne thermal emission and reflection radiometer (ASTER) satellite data are some of the most commonly adopted multispectral data for the mapping of hydrothermal alteration minerals. Compared to multispectral data, hyperspectral data have stronger ground object recognition ability. Chinese Gaofen-5 (GF-5) is the first hyperspectral satellite independently developed by China that has the advantages of both wide-width and high-spectral-resolution technology. However, the mapping ability of GF5 data for hydrothermal alteration minerals requires further study. In this study, ASTER and GF-5 satellite data were implemented to map hydrothermal alteration minerals in the Longtoushan Pb-Zn deposit, SW China. Selective principal component analysis (SPCA) technology was employed to map iron oxide/hydroxides, argillic, quartz, and carbonate minerals at the pixel level using ASTER data, and the mixture tuned matched filtering (MTMF) method was implemented for the extracted hematite, kaolinite, calcite, and dolomite at the sub-pixel level using GF-5 data. When mapping the hydrothermal alteration minerals, the distribution features of the hydrothermal alteration minerals from the Longtoushan Pb-Zn deposit were systematically revealed. A comprehensive field investigation and petrographic study were conducted to verify the extraction accuracy of the hydrothermal alteration minerals. The results showed that the overall accuracies for the ASTER and GF-5 data were 82.6 and 92.9 and that the kappa coefficients were 0.78 and 0.90, respectively. This indicates that the GF-5 data are able to map hydrothermal alteration minerals well and that they can be promoted as a hyperspectral data source for mapping systematic hydrothermal alteration minerals in the future.

Highlights

  • IntroductionHydrothermal alteration minerals, key indicators of hydrothermal deposit mineralization, are effective prospecting indicators

  • ASTER and GF-5 satellite data were utilized to map the hydrothermal alteration minerals associated with Pb-Zn mineralization in the Longtoushan deposit

  • This study strongly suggests that the GF-5 data are able to map hydrothermal alteration minerals well and that it can be promoted as a hyperspectral data source for future systematic hydrothermal alteration mineral mapping

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Summary

Introduction

Hydrothermal alteration minerals, key indicators of hydrothermal deposit mineralization, are effective prospecting indicators. Since remote sensing technology has the advantages of being speedy and cost-effective, multi-source remote sensing satellite data, including multispectral and hyperspectral data, are applied to various hydrothermal deposits for prospect exploration around the world [1–13]. The most commonly adopted multispectral satellite data for hydrothermal alteration minerals mapping are advanced spaceborne thermal emission and reflection radiometer (ASTER) data [14–20]. The visible and near-infrared (VNIR) bands of the ASTER satellite data and their shortwave infrared (SWIR) bands are utilized to map iron oxides/hydroxides and argillic, phyllic, and carbonate minerals in a number of published papers [21–24]. Thermal infrared (TIR) bands are applied for silicified alteration identification [25–29]

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