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Analysis of VIS-LWIR hyperspectral image data for detailed geologic mapping

机译:分析VIS-LWIR高光谱图像数据以进行详细的地质制图

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摘要

Research is being conducted into the usefulness of hyperspectral data for detailed geologic mapping applications. The data being analyzed were collected by the HYDICE (VIS-SWER) and SEBASS (LWIR) airborne imaging spectrometers. Hyperspectral data provides a means of identifying surface mineralogy, which indicates lithology. In addition, because the data are collected in image format, photo-geologic observations can be made, such as the presence and orientation of stratification and faulting. The results of hyperspectral-based geologic mapping are summarized for an area of volcanic and sedimentary rocks in southwest Nevada. Analysis of the data revealed 11 mineral endmembers representing eight lithologic units. The hyperspectral-derived maps were directly compared to the best ground-based geologic maps available. Results indicate the ability to produce general geologic maps at scales better than 1:24,000 using l-meter resolution airborne spectroscopy. Also, a more thorough mapping was achieved because of the increased compositional information gained by using both the SWIR and LWIR.
机译:目前正在研究高光谱数据对详细地质制图应用的有用性。通过HYDICE(VIS-SWER)和SEBASS(LWIR)机载成像光谱仪收集正在分析的数据。高光谱数据提供了识别表层矿物学的手段,这表明了岩性。另外,由于数据是以图像格式收集的,因此可以进行光地质观测,例如分层和断层的存在和方向。概述了内华达州西南部火山岩和沉积岩地区基于高光谱的地质测绘结果。对数据的分析显示出代表八个岩性单元的11个矿物端构件。直接将高光谱地图与现有的最佳地面地质地图进行比较。结果表明,使用l米分辨率机载光谱仪,可以生成比例尺大于1:24,000的一般地质图。另外,由于同时使用SWIR和LWIR获得的成分信息增加,因此实现了更彻底的映射。

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