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The Saxo-Danubian granite belt: magmatic response to postcollisional delamination of mantle lithosphere the south-western sector of the Bohemian Massif (Variscan orogen)
- 1.0330965 - ÚSMH 2010 RIV SK eng J - Journal Article
Finger, F. - Gerdes, A. - René, Miloš - Riegler, G.
The Saxo-Danubian granite belt: magmatic response to postcollisional delamination of mantle lithosphere the south-western sector of the Bohemian Massif (Variscan orogen).
[Sasko-dunajské granitové pásmo: magmatická odezva postkolizní delaminace plášťové litosféry pod jihozápadní částí Českého masívu (variský orogén).]
Geologica Carpathica. Roč. 60, č. 3 (2009), s. 205-212. ISSN 1335-0552. E-ISSN 1336-8052
R&D Projects: GA MŠMT MEB060802
Institutional research plan: CEZ:AV0Z30460519
Keywords : Bohemian Massif * granite * delamination
Subject RIV: DB - Geology ; Mineralogy
Impact factor: 0.963, year: 2009
Based on the synchronicity of geochronological data and the similarity of granite types, it is proposed that the Erzgebirge Batholith in the Saxothuringian Zone and the South Bohemian Batholith in the Moldanubian Zone belong to one cogenetic plutonic megastructure.
Geochronologická data a podobnost složení granitů krušnohorského a moldanubického batolitu umožňují vymezit kogenetickou plutonickou megastrukturu.
Permanent Link: http://hdl.handle.net/11104/0176617
Number of the records: 1