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Model near‐infrared optical constants of olivine and pyroxene as a function of iron content

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Lucey, Paul G.·1998·Journal of Geophysical Research: Planets

Abstract

The imaginary coefficients of the complex index of refraction of olivine, low‐Ca orthopyroxene, and high‐Ca clinopyroxene are derived as a function of iron content and wavelength over the spectral region 0.4 to 2.5 μm from reflectance spectra of powders and Hapke radiative transfer theory. Reflectance spectra as a function of composition and grain size are computed and compared. I find that while spectral effects of variations in these parameters are similar, they are distinguishable. Variations in iron content do not explain all the observed spectral variations in the spectra of the samples investigated.

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Metadata

Authors
Lucey, P. G.
Venue
Journal of Geophysical Research: Planets
Published
1998-01
Volume
103
Issue
E1
Pages
1703-1713
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2092391376
Cited by
212
References
0
FWCI
3.02
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Model near‐infrared optical constants of olivine and pyroxene as a function of iron content. https://app.cochat.ai/papers/10.1029/97je03145
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Lucey, P. G. (1998). Model near‐infrared optical constants of olivine and pyroxene as a function of iron content. Journal of Geophysical Research: Planets. https://doi.org/10.1029/97je03145

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