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Bottom to top lithosphere structure and evolution of western Eger Rift (Central Europe)

SYSNO ASEP	0330752
Document Type	J - Journal Article
R&D Document Type	Journal Article
Subsidiary J	Článek ve WOS
Title	Bottom to top lithosphere structure and evolution of western Eger Rift (Central Europe)
Author(s)	Babuška, Vladislav (GFU-E)_{ORCID, RID, SAI} Fiala, Jiří (GLU-S)_{SAI, RID} Plomerová, Jaroslava (GFU-E)_{ORCID, RID, SAI}
Source Title	International Journal of Earth Sciences. - : Springer - ISSN 1437-3254 Roč. 99, č. 4 (2010), s. 891-907
Number of pages	17 s.
Language	eng - English
Country	DE - Germany
Keywords	western Bohemian Massif ; Eger (Ohře) Rift ; lithosphere structure and development ; mantle seismic anisotropy
Subject RIV	DC - Siesmology, Volcanology, Earth Structure
R&D Projects	GA205/07/1088 GA ČR - Czech Science Foundation (CSF)
	IAA300120709 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
CEZ	AV0Z30120515 - GFU-E (2005-2011)
	AV0Z30130516 - GLU-S (2005-2011)
UT WOS	000277641600011
DOI	10.1007/s00531-009-0434-4
Annotation	We present model of the structure and development of the entire lithosphere beneath the western Eger Rift (ER). Its crustal architecture and paths of volcanic products are closely related to sutures/boundaries of uppermost mantle domains distinguished by different orientations of olivine fabric, derived from 3-D analysis of seismic anisotropy. Three different fabrics of the mantle lithosphere belong to the Saxothuringian (ST), Teplá-Barrandian (TB) and Moldanubian (MD) microplates assembled during the Variscan orogeny. Dipping fossil (pre-assembly) olivine orientations, consistent within each unit, do not support any voluminous mantle delamination.
Workplace	Geophysical Institute
Contact	Hana Krejzlíková, kniha@ig.cas.cz, Tel.: 267 103 028
Year of Publishing	2011

Number of the records: 1