Deciphering the Variscan tectonothermal overprint and deformation partitioning in the Cadomian basement of the Teplá–Barrandian unit, Bohemian Massif-Reference-Cited by-同舟云学术

Deciphering the Variscan tectonothermal overprint and deformation partitioning in the Cadomian basement of the Teplá–Barrandian unit, Bohemian Massif

Published:2012-02-24 Issue:7 Volume:101 Page:1855-1873
ISSN:1437-3254
Container-title:International Journal of Earth Sciences
language:en
Short-container-title:Int J Earth Sci (Geol Rundsch)

Author:

Hajná Jaroslava,Žák Jiří,Kachlík Václav,Chadima Martin

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Link

http://link.springer.com/content/pdf/10.1007/s00531-012-0753-8.pdf

Reference98 articles.

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4. Burg JP (1999) Ductile structures and instabilities: their implication for Variscan tectonics in the Ardennes. Tectonophysics 309:1–25

5. Čech S, Havlíček V, Zikmundová J (1988) Upper Devonian and Lower Carboniferous in north-eastern Bohemia (based on boreholes in the Hradec Králové area). Bull Central Geol Surv 64:65–75

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