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Thermal infrared (2.5-13.5 ??m) spectroscopic remote sensing of igneous rock types on particulate planetary surfaces

Journal of Geophysical Research

By:
and

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Abstract

Mineralogical information is retained in overtones and combination tones of the fundamental molecular vibrations in the 3.0-7.0 ??m region, but relatively few minerals have a sufficiently distinctive band structure to be unambiguously identified with currently available techniques. More significantly, identification of general rock type, as defined by the SCFM chemical index (SCFM = SiO2/SiO2 + CaO + FeO + MgO), is possible using spectral features associated with the principal Christiansen frequency and with a region of relative transparency between the Si-O stretching and bending bands. However, environmental factors may affect the appearance and wavelengths of these features. -from Authors

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Thermal infrared (2.5-13.5 ??m) spectroscopic remote sensing of igneous rock types on particulate planetary surfaces
Series title:
Journal of Geophysical Research
Volume
94
Issue:
B7
Year Published:
1989
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Journal of Geophysical Research
First page:
9192
Last page:
9202