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首页> 外文期刊>ISPRS Journal of Photogrammetry and Remote Sensing >Enhanced detection of gossans using hyperspectral data: Example from the Cape Smith Belt of northern Quebec, Canada
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Enhanced detection of gossans using hyperspectral data: Example from the Cape Smith Belt of northern Quebec, Canada

机译:使用高光谱数据增强对流浪者的检测:以加拿大魁北克省北部的史密斯角带为例

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Owing to the links between gossans and mineral deposits, detecting gossans by remote sensing means is essential for mineral exploration. In northern regions, gossans can develop as thin oxidized surfaces, named thin gossans, that can be covered with lichens. This study investigates the effects of spectral mixing between such gossans with lichens and their rock substrates using laboratory spectroscopic data obtained from samples collected in the Cape Smith Belt of Canada. These observations are then scaled up to the airborne hyperspectral data obtained from the same area. Our laboratory results indicate that the presence of lichens on gossans induces a general spectral shift towards shorter wavelengths of the iron absorption typical of gossan spectra. The opposite shift is observed due to the influence of the rock substrates. These effects can thus impede classification of gossans based on the interpretation of iron oxide mineralogy from spectra. Our airborne spectral results suggest that thin gossans can be detected and discriminated from thick gossans, and further broken down into several classes according to their host rock substrates. The ability to define distinct classes of thin gossans is significant since the association of these gossans with specific rock substrates can be exploited for exploration. The ability to distinguish thin and thick gossans alone can contribute to mineral exploration since it can be either the former or the latter group of gossans that acts as an ore deposit vector. (C) 2016 International Society for Photogrammetry and Remote Sensing, Inc. (ISPRS). Published by Elsevier B.V. All rights reserved.
机译:由于高棉岩和矿床之间的联系,通过遥感手段探测高棉岩对矿物勘探至关重要。在北部地区,棉布可以形成薄的氧化表面,称为薄棉布,可以被地衣覆盖。这项研究使用从加拿大海角史密斯带收集的样本获得的实验室光谱数据,研究了此类带有地衣的棉布和它们的岩石基质之间的光谱混合效应。然后将这些观测结果按比例放大到从同一地区获得的机载高光谱数据。我们的实验室结果表明,在棉球上存在地衣会导致一般的光谱向典型的棉球光谱中铁吸收的较短波长移动。由于岩石基质的影响,观察到相反的偏移。因此,这些影响可能会妨碍光谱仪根据光谱对氧化铁矿物学的解释来分类戈桑。我们的机载光谱结果表明,可以检测到薄的戈桑并将其与厚的戈桑进行区分,并根据其宿主岩石基质将其进一步细分为几类。定义不同类别的薄壁厚壁的能力非常重要,因为可以将这些壁厚与特定岩石基质的关联进行勘探。单独区分稀薄的和厚的棉纱的能力可以促进矿物勘探,因为它可以是前一组或后一组棉纱充当矿石沉积载体。 (C)2016国际摄影测量与遥感学会(ISPRS)。由Elsevier B.V.发布。保留所有权利。

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