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Majer, Vladimir, Mason, Roger (1983) High-pressure metamorphism between the pelagonian Massif and Vardar Ophiolite Belt, Yugoslavia. Mineralogical Magazine, 47 (343) 139-141 doi:10.1180/minmag.1983.047.343.03

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Reference TypeJournal (article/letter/editorial)
TitleHigh-pressure metamorphism between the pelagonian Massif and Vardar Ophiolite Belt, Yugoslavia
JournalMineralogical MagazineISSN0026-461X
AuthorsMajer, VladimirAuthor
Mason, RogerAuthor
Year1983 (June)Volume47
Issue343
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_47/47-343-139.pdf+
DOIdoi:10.1180/minmag.1983.047.343.03Search in ResearchGate
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Mindat Ref. ID3493Long-form Identifiermindat:1:5:3493:1
GUID0
Full ReferenceMajer, Vladimir, Mason, Roger (1983) High-pressure metamorphism between the pelagonian Massif and Vardar Ophiolite Belt, Yugoslavia. Mineralogical Magazine, 47 (343) 139-141 doi:10.1180/minmag.1983.047.343.03
Plain TextMajer, Vladimir, Mason, Roger (1983) High-pressure metamorphism between the pelagonian Massif and Vardar Ophiolite Belt, Yugoslavia. Mineralogical Magazine, 47 (343) 139-141 doi:10.1180/minmag.1983.047.343.03
In(1983, June) Mineralogical Magazine Vol. 47 (343) Mineralogical Society
Abstract/NotesAbstractA 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.


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