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European Journal of Mineralogy; March, April 2003; v. 15; no. 2; p. 365-371; DOI: 10.1127/0935-1221/2003/0015-0365
© 2003 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Articles

The structure of Pbca orthopyroxenes along the join diopside-enstatite (CaMgSi2O6-Mg2Si2O6)

Fabrizio NESTOLA and Mario TRIBAUDINO*

Dipartimento di Scienze Mineralogiche e Petrologiche, Università di Torino, Via Valperga Caluso 35, I-10125 Torino, Italy

* e-mail: mario.tribaudino{at}unito.it

The crystal structure of two synthetic orthopyroxenes, with compositions Ca0.04Mg1.96Si2O6 and Ca0.07Mg1.93Si2O6 has been refined by single-crystal X-ray diffraction [R(4{sigma}) = 2.7 and 3.6 %, respectively]. TEM observation has shown the presence of irregularly repeated P21/c clinopyroxene lamellae, oriented parallel to (100), in agreement with the presence of reflections with 1 = 2n violating the b glide plane.

Significant electron density residuals close to the M2 and O2B sites were found, allowing split site refinement for the sample with composition Ca0.07Mg1.93Si2O6. M2-O bond lengths for average and local configurations for Ca and Mg have been found to be very similar to those of clinopyroxenes along the join diopside-enstatite. The increasing presence, due to the substitution of Ca for Mg in the M2 site, of Ca configurations in orthopyroxene that are similar to the average ones in Ca-richer C2/c clinopyroxene reduces the stability of the orthopyroxene phase.

Key-words: orthopyroxene, split site refinement, diopside-enstatite, crystal structure, X-ray single-crystal diffraction..




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