C. Koike et al., EXTINCTION OF OLIVINE AND PYROXENE IN THE MIDINFRARED AND FAR-INFRARED, Monthly Notices of the Royal Astronomical Society, 264(3), 1993, pp. 654-658
The extinction coefficients Q(ext)/a of orthopyroxene, clinopyroxene,
Fo100, Fo90, Fo80, Fo60, Fo40 and the Allende meteorite have been obta
ined in the mid- and far-infrared ranges. These crystalline silicates
have many absorption peaks. The main peaks in forsterite at 10, 11, 20
, 24, 34, 50 and 70 mum shift to longer wavelength and weaken as the M
g/(Mg + Fe) ratio decreases. We discuss the composition of cometary du
st grains in relation to our data.