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High-pressure metamorphism between the pelagonian Massif and Vardar Ophiolite Belt, Yugoslavia

Published online by Cambridge University Press:  05 July 2018

Vladimir Majer  and
Roger Mason
Vladimir Majer
Affiliation:
Institute for Mineralogy, Petrology, and Economic Geology, Faculty of Mining, Geology, and Petroleum Engineering, University of Zagreb, PO Box 186, 41000 Zagreb, Yugoslavia
Roger Mason
Affiliation:
Institute for Mineralogy, Petrology, and Economic Geology, Faculty of Mining, Geology, and Petroleum Engineering, University of Zagreb, PO Box 186, 41000 Zagreb, Yugoslavia
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Abstract

A reported occurrence of metamorphic rocks containing sodic pyroxenes, in the transition zone between the Pelagonian Crystalline Massif and the Vardar Ophiolite Belt, in Macedonia, Yugoslavia, has been re-investigated, and pyroxenes, micas, plagioclase, and clinozoisite analysed by microprobe. The presence of the high-pressure metamorphic assemblage quartz + omphacite+albite is confirmed, giving the first definite indication of blueschist-facies metamorphic conditions in Yugoslavia.

Type
Research Article
Information
Mineralogical Magazine , Volume 47 , Issue 343 , June 1983 , pp. 139 - 141
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1983

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