Add to ORKGⅠ. THE MIDDLE INFRARED SPECTRAL REFLECTANCE CHARACTERISTICS OF CARBONATE ROCKS The middle infrared reflective spectral response curves for the minerals of carbonate rocks are usually fairly distinct, and the spectral reflectance characteristic crests of the minerals from different areas are appr...04502-50
Diatomite, a rock formed by the accumulation of opaline diatom frustules, is a preferred raw materia...
Terrestrial rock compositions can be defined by the shift in wavelength of the fundamental Si-O vibr...
In spite of extensive search carbonates have not been found until nowon the Martian surface by spect...
Typescript.Thesis (Ph. D.)--University of Hawaii at Manoa, 1984.Bibliography: leaves 219-236.Microfi...
Reflectance spectra of carbonate minerals in the shortwave infrared (SWIR) and thermal infrared (TIR...
Abstract: Reflectance spectra of carbonate minerals in the shortwave infrared (SWIR) and thermal inf...
Reflectance spectroscopy in the visible and near-infrared (VNIR) is a common technique used to study...
This study presents far infrared spectra in the range 650-70 cm -1 of 18 common and rare carbonate m...
This study presents far infrared spectra in the range 650-70 cm(-1) of 18 common and rare carbonate ...
A carbonate (CO3) prediction model was developed for soils throughout the contiguous United States u...
Diatomite, a rock formed by the accumulation of opaline diatom frustules, is a preferred raw materia...
The middle infrared portion of the spectrum available for geologic remote sensing extends from appro...
The objective of the present study was to determine the predominant minerals in sedimentary rocks us...
ABSTRACT. Results from a remote sensing study on the spectral reflectance of intermediate igneous ro...
The author has identified the following significant results. Visible and near-infrared (0.35 to 2.5 ...
Diatomite, a rock formed by the accumulation of opaline diatom frustules, is a preferred raw materia...
Terrestrial rock compositions can be defined by the shift in wavelength of the fundamental Si-O vibr...
In spite of extensive search carbonates have not been found until nowon the Martian surface by spect...
Typescript.Thesis (Ph. D.)--University of Hawaii at Manoa, 1984.Bibliography: leaves 219-236.Microfi...
Reflectance spectra of carbonate minerals in the shortwave infrared (SWIR) and thermal infrared (TIR...
Abstract: Reflectance spectra of carbonate minerals in the shortwave infrared (SWIR) and thermal inf...
Reflectance spectroscopy in the visible and near-infrared (VNIR) is a common technique used to study...
This study presents far infrared spectra in the range 650-70 cm -1 of 18 common and rare carbonate m...
This study presents far infrared spectra in the range 650-70 cm(-1) of 18 common and rare carbonate ...
A carbonate (CO3) prediction model was developed for soils throughout the contiguous United States u...
Diatomite, a rock formed by the accumulation of opaline diatom frustules, is a preferred raw materia...
The middle infrared portion of the spectrum available for geologic remote sensing extends from appro...
The objective of the present study was to determine the predominant minerals in sedimentary rocks us...
ABSTRACT. Results from a remote sensing study on the spectral reflectance of intermediate igneous ro...
The author has identified the following significant results. Visible and near-infrared (0.35 to 2.5 ...
Diatomite, a rock formed by the accumulation of opaline diatom frustules, is a preferred raw materia...
Terrestrial rock compositions can be defined by the shift in wavelength of the fundamental Si-O vibr...
In spite of extensive search carbonates have not been found until nowon the Martian surface by spect...