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Clinopyroxene exsolution in wollastonite from Namaqualand granulite, South Africa

  • Yusuke Seto EMAIL logo , Shugo Ohi , Norimasa Shimobayashi , Masao Kitamura , Akira Miyake , Yoshikuni Hiroi and Geoffrey H. Grantham
Published/Copyright: March 31, 2015
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Abstract

Chemical and crystallographic properties of clinopyroxene exsolution in wollastonite are described from metamorphosed calc-silicate granulite, Namaqualand, South Africa. The wollastonite is Ca1.96Fe0.01Al0.01Si2.01-O6 belonging to space group P21/a (2M polytype) and the clinopyroxene is Ca0.99Mg0.75-0.80Fe0.17-0.21Na0.02Al0.03Si1.99-2.00O6 belonging to C2/c. An electron backscattered diffraction investigation suggests that the clinopyroxene lamellae elongated along [11̅1] lie on (120) and (100) of the wollastonite-2M, and [11̅0] of both lamellae are parallel to [001] of the wollastonite-2M. The formation of the exsolution probably results from the relatively high peak metamorphic temperature (800-860ºC) of the Namaqualand granulite and its slow cooling rate.

Received: 2005-8-16
Accepted: 2005-10-28
Published Online: 2015-3-31
Published in Print: 2006-2-1

© 2015 by Walter de Gruyter Berlin/Boston

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