Thermal Infrared Hyperspectral Imaging for Mineralogy Mapping of a Mine Face
ASTER mineral mapping examples
![PDF] Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite | Semantic Scholar](https://d3i71xaburhd42.cloudfront.net/c107f36b2bf12a5ed5e22b6b289eb669840cbdfd/7-Figure14-1.png "PDF] Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite | Semantic Scholar")
PDF] Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite | Semantic Scholar
How GeoSpectral Imaging™ works - TerraCore
Characterisation of carbonate minerals from hyperspectral TIR scanning using features at 14 000 and 11 300 nm
Visible and Near-Infrared Reflectance Spectroscopy (Chapter 4) - Remote Compositional Analysis
Hyperspectral remote sensing in lithological mapping, mineral exploration, and environmental geology: an updated review
VNIR SPECTRA OF GYPSUM-RICH FIELD SAMPLES FROM WHITE SANDS NEW MEXICO AS AN ANALOG STUDY FOR OLYUMPUS UNDAE, MARS. S. J. King1,
Visible and Near-Infrared Reflectance Spectroscopy (Chapter 4) - Remote Compositional Analysis
![PDF] Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite | Semantic Scholar](https://d3i71xaburhd42.cloudfront.net/c107f36b2bf12a5ed5e22b6b289eb669840cbdfd/7-Figure13-1.png "PDF] Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite | Semantic Scholar")
PDF] Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite | Semantic Scholar
a) Standard spectra from the USGS library in the VNIR and SWIR from... | Download Scientific Diagram
Calcite, dolomite, gypsum, illite, and kaolinite spectra from USGS... | Download Scientific Diagram
Shortwave infrared hyperspectral imaging as a novel method to elucidate multi-phase dolomitization, recrystallization, and cementation in carbonate sedimentary rocks | Scientific Reports
Remote Sensing | Free Full-Text | Application of ASTER Data for Differentiating Carbonate Minerals and Evaluating MgO Content of Magnesite in the Jiao-Liao-Ji Belt, North China Craton | HTML
![PDF] Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite | Semantic Scholar](https://d3i71xaburhd42.cloudfront.net/c107f36b2bf12a5ed5e22b6b289eb669840cbdfd/10-Figure15-1.png "PDF] Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite | Semantic Scholar")
PDF] Spectral reflectance of-carbonate minerals in the visible and near infrared (0.35-2.55 microns): calcite, aragonite, and dolomite | Semantic Scholar
Chapter TOC 1 2 3 4_5_6_7_8 nopics_refs_appendix
Laboratory reflectance spectra of hydrothermally altered carbonate facies, Pine Point mining camp, NWT, Canada | Geochemistry: Exploration, Environment, Analysis
ASTER and WorldView-3 satellite data for mapping lithology and alteration minerals associated with Pb-Zn mineralization
A New Band Ratio Approach for Discriminating Calcite and Dolomite by ASTER Imagery in Arid and Semiarid Regions | SpringerLink
