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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
- 1.Finger, F. - Gerdes, A. - René, Miloš
The Saxo-Danubian Granite Belt: A large scale magmatic structure revealing Late Variscan mantle tectonics below the south-western Bohemian Massif.
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.), s. 46-47. ISBN 978-3-910006-39-3.
[From Gondwana and Laurussia to Pangaea: Dynamics of Oceans and Supercontinents 20th International Senckenberg Conference and 2th Geinitz Conference. Frankfurt am Main (DE), 30.09.2008-03.10.2008]
http://hdl.handle.net/11104/0166294
Počet záznamů: 1