Hyperspectral remote sensing in lithological mapping, mineral exploration, and environmental geology: an updated review
Identification and composition of carbonate minerals of the calcite structure by Raman and infrared spectroscopies using portable devices - ScienceDirect
![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
Spectral features of calcite, dolomite, gypsum and anhydrite in the... | Download Scientific Diagram
VNIR SPECTRA OF GYPSUM-RICH FIELD SAMPLES FROM WHITE SANDS NEW MEXICO AS AN ANALOG STUDY FOR OLYUMPUS UNDAE, MARS. S. J. King1,
VNIR spectra of gypsum/dolomite mixtures. Gypsum features are clearly... | Download Scientific Diagram
Characterisation of carbonate minerals from hyperspectral TIR scanning using features at 14 000 and 11 300 nm
How GeoSpectral Imaging™ works - TerraCore
A New Band Ratio Approach for Discriminating Calcite and Dolomite by ASTER Imagery in Arid and Semiarid Regions | SpringerLink
ASTER mineral mapping examples
VNIR spectra of gypsum/dolomite mixtures. Gypsum features are clearly... | Download Scientific Diagram
Investigation of spectral characteristics of carbonate rocks – A case study on Posht Moleh Mount in Iran
![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
![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
Mineral Identification and Mapping by Synthesis of Hyperspectral VNIR/SWIR and Multispectral TIR Remotely Sensed Data With Diffe
Investigation of spectral characteristics of carbonate rocks – A case study on Posht Moleh Mount in Iran
ASTER and WorldView-3 satellite data for mapping lithology and alteration minerals associated with Pb-Zn mineralization
Tracing Carbonate Formation, Serpentinization, and Biological Materials With Micro‐/Meso‐Scale Infrared Imaging Spectroscopy in a Mars Analog System, Samail Ophiolite, Oman - Leask - 2021 - Earth and Space Science - Wiley Online Library
Remote Sensing | Free Full-Text | Application of Landsat-8, Sentinel-2, ASTER and WorldView-3 Spectral Imagery for Exploration of Carbonate-Hosted Pb-Zn Deposits in the Central Iranian Terrane (CIT) | HTML
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
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
Field-Portable VNIR Spectrometry: Applications for Mars Rover Operational Strategies Testing at Terrestrial Analog Sites
