用非线性高光谱解调技术鉴定火星上的基性矿物

A. Marinoni, H. Clenet
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引用次数: 4

摘要

通常,通过分析吸收特征的重叠,可以从光谱中获得火星矿物学的定量解释。通过应用适当的反褶积技术,例如基于修正高斯模型(MGM)的技术,可以实现对所考虑的场景中每种矿物的丰度的全面描述。然而,基于mgm的方法对统计分布定义的初始参数很敏感,或者在完全自动化的情况下非常耗时。本文介绍了一种利用高阶非线性高光谱分解框架识别火星表面矿物的新方法。根据多体分解算法反演岩浆矿物(橄榄石和辉石)化合物的丰度分布。实验结果表明,该方法能够提供实际丰度图,且丰度图与基于自动化mgm技术的丰度图高度相关。
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Identification of mafic minerals on Mars by nonlinear hyperspectral unmixing
Typically, quantitative interpretation of Mars mineralogy from spectra can be retrieved by analyzing the overlaps of absorption features. It is possible to achieve a thorough description of the abundances of each mineral the considered scene is composed of by applying proper deconvolution techniques such as those based on modified Gaussian model (MGM). However, MGM-based methods are sensitive on initial parameters for statistical distribution definition, or they are very time consuming when fully automatized. In this paper, a new method for identification of minerals on Mars surface by means of higher order nonlinear hyperspectral unmixing framework is introduced. Abundance distribution of magmatic minerals (olivine and pyroxenes) compounds is retrieved according to polytope decomposition algorithm. Experimental results show how the proposed method is able to provide actual abundance maps which are highly correlated to those obtained by an automatized MGM-based technique.
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