Pyroxene Visible Spectra (generally 350 - 2500 nm)
polarizations: (a = alpha direction; b = beta direction; g = gamma direction)
Pictures of pyroxenes showing the pleochroism
Enstatite polarized parallel to the c-axis; two crystals, one from Tanzania, the other from Myanmar
Enstatite polairzed parallel to the b-axis
Both, compared side-by-side
Images of representative orthopyroxene spectra
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enstatite image; Enstatite (bronzite,
Fs 14.0), GRR 40, Bamble, Norway, 0.100 mm thick with Fe2+ in
the M2 site dominating the spectrum. Data Files: alpha;
beta; gamma. Image of the alpha band on scale
(0.095 mm thick). Data File: alpha on scale
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enstatite image; Enstatite (hypersthene,
Fs 39.5), GRR 1653, Summit Rock, Oregon, 0.10 mm thick With type Fe2+
in the M2 site dominating the spectrum and a M1 site feature near 1200
nm. Data Files: alpha;
beta; gamma
Synthetic orthopyroxenes containing various transition elements.
Images of representative clinopyroxene spectra
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CIT 13748 image; Augite, GRR 583,
CIT 13748, Cedar Butte, Oregon, 0.10 mm thick with type Fe2+
in the M2 site dominating the spectrum. Data Files: alpha; beta;
gamma
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CIT 7524 image; Diopside, GRR
472, CIT 7524, Binntal Wallis, Switzerland, 0.50 mm thick. This shows both
Fe2+ and Fe2+ - Fe3+ intervalance charge
transfer. Data Files: alpha; beta; gamma
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RDS 62047-70 image; Diopside, chromian,
Russia, 1.00 mm thick. The band at 1030 nm is from Fe2+
whereas the other features are from Cr3+. The crystal contains
0.558 wt% Cr2O3. This was taken with light
polarized along each crystallographic axis. Data Files: E||b.
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Jadeite image; Jadeite from Kazakhstan,
polycrystalline mass run unpolarized and normalized to 10 mm thick.
The spectrum is dominated by Cr3+ but also shows the Fe3+
band near 440 nm. Data file: Contributed data from Anton Vasiliev,
LAL, Moscow: unpolarized.
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GRR 151 image; Spodumene, GRR 151,
lavendar colored kunzite variety, Pala, California, USA, 10.0 mm thick
showing Mn3+ features. Data Files: alpha not ready; beta not ready ; gamma not ready
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