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The Saxo-Danubian Granite Belt: A large scale magmatic structure revealing Late Variscan mantle tectonics below the south-western Bohemian Massif
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SYSNO ASEP 0316346 Document Type C - Proceedings Paper (int. conf.) R&D Document Type Conference Paper Title The Saxo-Danubian Granite Belt: A large scale magmatic structure revealing Late Variscan mantle tectonics below the south-western Bohemian Massif Title Saxo-danubienská granitová zóna: Významná magmatická struktura spjatá se stavbou variského pláště v jihozápadní části Českého masivu Author(s) Finger, F. (AT)
Gerdes, A. (DE)
René, Miloš (USMH-B) RID, ORCID, SAISource Title From Gondwana and Laurussia to Pangaea: Dynamics of Oceans and Supercontinents 20th International Senckenberg Conference and 2th Geinitz Conference. Final meeting of IGCP 497 and IGCP 499. Abstracts and Programe. - Frankfurt am Main : Senckenberg Forschungsinstitut und Naturmuseum, 2008 / Koenigshof P. ; Linnemann U. - ISBN 978-3-910006-39-3 Pages s. 46-47 Number of pages 2 s. Action From Gondwana and Laurussia to Pangaea: Dynamics of Oceans and Supercontinents 20th International Senckenberg Conference and 2th Geinitz Conference Event date 30.09.2008-03.10.2008 VEvent location Frankfurt am Main Country DE - Germany Event type WRD Language eng - English Country DE - Germany Keywords Bohemian Massif ; Moldanubian Zone ; granite Subject RIV DB - Geology ; Mineralogy R&D Projects MEB060802 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) CEZ AV0Z30460519 - USMH-B (2005-2011) Annotation Remarkable synchronicity of magma forming processes leads to the conclusion that the granite plutons of the Fichtelgebirge /Western Erzgebirge and the South Bohemian batholith can be combined to one coherent an cogenetic plutonic system. Workplace Institute of Rock Structure and Mechanics Contact Iva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216 Year of Publishing 2009
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