Raman spectra of several compositions of (Mg, Fe, Ca)SiO3 pyroxenes were co
llected at ambient conditions. More than 10 Raman vibrational modes were ob
served for these pyroxenes in the wavenumber range between 200 and 1200 cm(
-1). in general, these pyroxenes are characterized by (1) the Si-O stretchi
ng modes above 800 cm(-1); (2) the Si-O bending modes between 500 and 760 c
m(-1); (3) SiO4 rotation and metal-oxygen translation modes below 500 cm(-1
). For a constant Ca content, frequencies of the Raman modes in the enstati
te-ferrosilite (opx) and diopside-hedenbergite (cpx) series generally decre
ase with an increase in Fe content. This phenomenon is attributed to an inc
rease in both the bonding lengths and the reduced mass as Fe2+ is substitut
ed for Mg. However, two modes at similar to 900 cm(-1) in the enstatite-fer
rosilite series increase in frequencies as Fe content increases. A possible
explanation is to the shortening in the Si-O-Si bridging bonding bonds whe
n the M2 sites are preferentially occupied by the iron cation. The effect o
f Fe substituting for Mg on the frequency shift in cpx is less profound tha
n opx because the larger M2 was occupied by calcium and the substitution of
iron and magnesium in the M1 site results in a less significant change in
the bond length. The major-element composition of the (Mg, Fe, Ca)-pyroxene
s, especially the orthopyroxene series, can be semi-quantitatively determin
ed on the basis of the peak positions of their characteristic Raman modes.