Pre-tertiary blueschist terrains in the Hellenides: Evidence from detrital minerals of flysch successions

dc.contributor.author	Faupl, P	en
dc.contributor.author	Pavlopoulos, A	en
dc.contributor.author	Wagreich, M	en
dc.contributor.author	Migiros, G	en
dc.date.accessioned	2014-06-06T06:43:12Z
dc.date.available	2014-06-06T06:43:12Z
dc.date.issued	1996	en
dc.identifier.issn	09544879	en
dc.identifier.uri	http://62.217.125.90/xmlui/handle/123456789/1084
dc.relation.uri	http://www.scopus.com/inward/record.url?eid=2-s2.0-0029751659&partnerID=40&md5=ae84ea5a16216f55a07215e5e76a3578	en
dc.subject.other	amphibole	en
dc.subject.other	blueschist	en
dc.subject.other	exhumation history	en
dc.subject.other	flysch	en
dc.subject.other	uplift	en
dc.subject.other	Greece, Hellenides	en
dc.title	Pre-tertiary blueschist terrains in the Hellenides: Evidence from detrital minerals of flysch successions	en
heal.type	journalArticle	en
heal.publicationDate	1996	en
heal.abstract	Detrital blue amphiboles detected in flysch sandstones of the Hellenides of mainland Greece give important information on uplift and exhumation history of blueschist terrains. The occurrence of these HP/LT minerals in the terminal flysch of the Pindos zone as well as in the Othrys flysch of the Subpelagonian zone from late Maastrichtian/ Palaeocene time onwards proves a Pre-Tertiary (Eohellenic) stage of blueschist formation. Detrital blue amphiboles from flysch sequences of the Ionian zone indicate a further pulse of uplift of high-pressure rocks during the Palaeocene/Eocene. Blueschist rocks of this latter time range are radiometrically well documented in the Hellenides.	en
heal.journalName	Terra Nova	en
dc.identifier.issue	2	en
dc.identifier.volume	8	en
dc.identifier.spage	186	en
dc.identifier.epage	190	en