ZIRCON STUDY FROM THE RHODOPE METAMORPHIC PROVINCE, GREECE

BAUER, C; KRENN, K; PERRAKI, M; HOINKES, G; Franzens, K

dc.contributor.author	BAUER, C	en
dc.contributor.author	KRENN, K	en
dc.contributor.author	PERRAKI, M	en
dc.contributor.author	HOINKES, G	en
dc.contributor.author	Franzens, K	en
dc.date.accessioned	2014-03-01T01:54:23Z
dc.date.available	2014-03-01T01:54:23Z
dc.date.issued	2005	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/27362
dc.relation.uri	http://www.uni-graz.at/IEC-7/PDF-files/Bauer.pdf	en
dc.subject	Information Gain	en
dc.subject	Raman Spectroscopy	en
dc.subject	Scanning Electron Microscopy	en
dc.title	ZIRCON STUDY FROM THE RHODOPE METAMORPHIC PROVINCE, GREECE	en
heal.type	journalArticle	en
heal.publicationDate	2005	en
heal.abstract	The Kimi complex of the northern Rhodope Metamorphic Province, Greece, is considered to be a proven ultrahigh-pressure unit since the presence of tiny (3 - 9 µm) microdiamond inclu- sions in metapelitic garnets was proven by Micro Raman Spectroscopy (PERRAKI et al., 2004). Zircons, known as containers of UHP minerals, were investigated from this area with Micro Raman Spectroscopy and	en