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Using Long wave Infrared Spectroscopy to Determine Changes in the Mafic Mineralogy of Drill Core Samples from the Humu'ula Groundwater Research Project

机译:使用长波红外光谱法测定Humu'ulu-Groundwater研究项目钻孔芯样品镁铁矿物学的变化

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Spectroscopy can be used effectively in the first stages of mineral identification and exploration. Long wave infrared (LWIR) wavelengths are particularly useful in identifying diagnostic features in common rock forming minerals. These techniques will be utilized to determine mafic minerology of eleven rock slabs from a drill core project in the Humu'ula Saddle region. Changes in the minerology of core samples through spectral shifts and changes in the long wave infrared will expand on our knowledge of geologic processes in the area as well as provide analogues to Mars. With widespread occurrences of mafic basaltic flows on the surface of Mars, critical examination of the minerology of Hawaiian drill core can help to model mafic and groundwater interactions on that planet. The results of this study will supplement previous studies of the drill core and offer insight into how long-wave infrared spectroscopy can complement data from shorter wavelengths.
机译:光谱可在矿物质识别和勘探的第一阶段有效使用。长波红外(LWIR)波长特别有用用于识别共同岩石形成矿物质中的诊断特征。这些技术将用于确定Humu'ula Saddle区域的钻芯项目的11岩石板的MAFIC型号。通过光谱移位和长波红外线的变化的核心样本的更改将扩大我们对该地区地质过程的知识以及为火星提供类似物。凭借在火星表面上广泛发生的MAFIC玄武岩流动,对夏威夷钻井核心的少校的临界检查可以帮助模拟该行星上的MAFIC和地下水相互作用。本研究的结果将补充对钻头核心的先前研究,并介绍了长波红外光谱如何将数据与较短波长的数据补充。

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