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An Andean type Palaeozoic convergence in the Bohemian Massif

SYSNO ASEP	0323890
Document Type	J - Journal Article
R&D Document Type	Journal Article
Subsidiary J	Článek ve WOS
Title	An Andean type Palaeozoic convergence in the Bohemian Massif
Title	Andský typ paleozoické konvergence v Českém masívu
Author(s)	Schulmann, K. (FR) Konopásek, J. (CZ) Janoušek, V. (CZ) Lexa, O. (CZ) Lardeaux, J.-M. (FR) Edel, J.-B. (FR) Štípská, P. (FR) Ulrich, Stanislav (GFU-E)
Source Title	Comptes Rendus Geoscience. - : Elsevier - ISSN 1631-0713 Roč. 341, č. 2-3 (2009), s. 266-286
Number of pages	21 s.
Language	eng - English
Country	NL - Netherlands
Keywords	Bohemian Massif ; Saxothuringian oceanic subduction ; building of Variscan orogenic root system ; channel flow
Subject RIV	DC - Siesmology, Volcanology, Earth Structure
CEZ	AV0Z30120515 - GFU-E (2005-2011)
UT WOS	000265225000014
DOI	10.1016/j.crte.2008.12.006
Annotation	The geological inventory of the Variscan Bohemian Massif can be summarized as a result of Early Devonian subduction of the Saxothuringian ocean of unknown size underneath the eastern continental plate represented by the present-day Teplá-Barrandian and Moldanubian domains. During mid-Devonian, the Saxothuringian passive margin sequences and relics of Ordovician oceanic crust have been obducted over the Saxothuringian basement in conjunction with extrusion of the Teplá-Barrandian middle crust along the so-called Teplá suture zone. This event was connected with the development of the magmatic arc further east, together with a fore-arc basin on the Teplá-Barrandian crust.
Workplace	Geophysical Institute
Contact	Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
Year of Publishing	2009

Number of the records: 1