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Rock type identification and abundance estimation from hyperspectral analysis.

机译:岩石类型识别和高光谱分析的丰度估算。

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摘要

This study explores the usefulness of hyperspectral data to discriminate rock units and estimate the abundance of sulfides in rocks. Airborne visible-near infrared (VIS-NIR) hyperspectral data collected from northern Cape Smith, Quebec and laboratory thermal infrared reflectance (TIR) data measured on rock samples from eight different mines in the Sudbury Basin, Ontario are involved in the analysis. The study addressed four different geological application scenarios with the aim of retrieving useful lithological information from rock spectra while minimizing the influence of varying environmental factors.; The research first examines the effects of topography on the selection of rock endmembers from airborne VIS_NIR spectra and demonstrates how a topographic correction process can improve the discrimination of rock units. It demonstrates that traditional ways of selecting spectral endmembers from hyperspectral data for areas of rugged terrain cannot provide representative rock unit signatures. The second part of the research targeted the mapping of wall rock in an underground environment using TIR spectra. Rock samples from mines of the Sudbury Basin in Ontario were measured using naturally broken surfaces both dry and wet to address environmental conditions encountered underground. An innovative method applying a spectral angle mapper on the 2nd derivative of rock spectra from 700--1300 cm-1 was proved to be robust to remove the effect of liquid water, local geometry and disseminated sulfide ores while preserving diagnostic rock signatures for mapping. The study then focuses on retrieving sulfide information from TIR to estimate ore (total sulfide abundance) grade on naturally broken rock faces and separate ore-bearing rocks from their host rocks in an underground environment regardless of rock types. An important finding is that reflectance at 1319 cm -1, where most silicate rocks demonstrate low reflectance, is related to total sulfide concentration in rocks. Finally, a study was conducted on core and cut rock faces to examine the usefulness of TIR in detecting sulfide ore zones and estimating total sulfide content in cores and cut rocks. Adaptable mathematical models were established and tested for potential core logging applications.; The most important result of this research is that rock spectra can be used to identify different rock types in an underground environment and on surface exposures in the field. Total sulfide content can be detected and predicted on naturally broken and cut rock faces using hyperspectral data.
机译:这项研究探索了高光谱数据用于区分岩石单元和估计岩石中硫化物含量的有用性。分析涉及从魁北克史密斯角北部收集的机载可见光近红外(VIS-NIR)高光谱数据以及对来自八个不同矿山的岩石样品测得的实验室热红外反射率(TIR)数据。该研究针对四种不同的地质应用场景,旨在从岩石光谱中检索有用的岩性信息,同时最大程度地减少各种环境因素的影响。该研究首先研究了地形对从机载VIS_NIR光谱中选择岩石端构件的影响,并证明了地形校正过程如何改善岩石单元的判别力。它表明,从崎spec的地形区域的高光谱数据中选择光谱末端成员的传统方法无法提供代表性的岩石单元特征。研究的第二部分针对使用TIR光谱绘制地下环境中的围岩图。安大略省萨德伯里盆地矿山的岩石样品使用干燥和潮湿的自然破碎表面进行了测量,以解决地下遇到的环境条件。一种新颖的方法将光谱角度映射器应用于700--1300 cm-1的岩石光谱的二阶导数,被证明在消除诊断中的岩性特征的同时,能够可靠地消除液态水,局部几何形状和分散的硫化矿石的影响。然后,研究集中于从TIR检索硫化物信息,以估计自然破碎岩石表面上的矿石(总硫化物丰度)品位,并在地下环境中将含矿岩石与它们的宿主岩石分开,而不论岩石类型如何。一个重要发现是,在大多数硅酸盐岩石反射率较低的1319 cm -1处的反射率与岩石中总硫化物浓度有关。最后,对岩心和切屑岩面进行了研究,以检验TIR在检测硫化物矿带和估算岩心和切屑岩中总硫化物含量方面的有用性。建立了适用的数学模型,并针对潜在的核心测井应用进行了测试。这项研究的最重要结果是,岩石光谱可用于识别地下环境和野外地面暴露中的不同岩石类型。可以使用高光谱数据在自然破碎和切割的岩石面上检测和预测总硫化物含量。

著录项

  • 作者

    Feng, Jilu.;

  • 作者单位

    University of Alberta (Canada).;

  • 授予单位 University of Alberta (Canada).;
  • 学科 Geology.; Geophysics.; Remote Sensing.
  • 学位 Ph.D.
  • 年度 2002
  • 页码 172 p.
  • 总页数 172
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 地质学;地球物理学;遥感技术;
  • 关键词

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