THE FORMATION OF GNEISSES IN THE SOUTHERN EAST URALIAN ZONE-A RESULT OF LATE PALAEOZOIC GRANITE ASCENT AND EMPLACEMENT

Görz I.; Kroner U.; Ivanov K.S.

dc.contributor.author	Görz I.
dc.contributor.author	Kroner U.
dc.contributor.author	Ivanov K.S.
dc.date.accessioned	2024-12-22T03:48:02Z
dc.date.available	2024-12-22T03:48:02Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13515632
dc.identifier.citation	Journal of Asian Earth Sciences, 2006, 27, 4, 402-415
dc.identifier.issn	1367-9120
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/47090
dc.description.abstract	Geochemical and radiogenic age data are incompatible with the idea that the gneiss-complexes of the East Uralian Zone are microcontinental blocks that collided with the Magnitogorsk island arc during the Uralian orogeny. Field and microstructural data from the Dzhabyk and Suunduk complexes presented in this paper enable us to suggest an alternative model that interprets the gneisses as deformed margins of the batholiths of the Uralian Granite Axis. The gneisses have been formed from a granitic protolith by a continuous fabric transformation on a retrograde metamorphic path. All structures in the gneisses can be assigned to the ascent and emplacement of batholiths in an active strike-slip belt. © 2005 Elsevier Ltd. All rights reserved.
dc.subject	EAST URALIAN ZONE
dc.subject	GRANITE-GNEISS COMPLEXES
dc.subject	MAGMA ASCENT
dc.subject	METAMORPHISM
dc.title	THE FORMATION OF GNEISSES IN THE SOUTHERN EAST URALIAN ZONE-A RESULT OF LATE PALAEOZOIC GRANITE ASCENT AND EMPLACEMENT
dc.type	Статья
dc.identifier.doi	10.1016/j.jseaes.2005.02.007