Ductile normal faulting along the West Bohemian Shear Zone (Moldanubian/Tepla-Barrandian boundary): Evidence for late Variscan extensional collapse in the Variscan Internides

Author:

Zulauf G.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference94 articles.

1. Andrusov D, Corna O (1976) Über das Alter des Moldanubikums nach mikrofloristischen Untersuchungen. Geol Prace, Spr 65: 81–89

2. Aranguren A, Tubia JM (1992) Structural evidence for the relationship between thrusts, extensional faults and granite intrusions in the Variscan belt of Galicia (Spain). J Struct Geol 14: 1229–1237

3. Beard BL, Medaris LG, Johnson CM, Misar Z, Jelinek E (1991) Nd and Sr isotope geochemistry of Moldanubian eclogites and garnet peridotites, Bohemian Massif, Czechoslovakia. Second Eclogite Field Symp, Terra Abstr, Abstr Suppl Terra Nova 3: 4

4. Behrmann JH (1988) Crustal-scale extension in a convergent orogen: the Sterzing-Steinach mylonite zone in the Eastern Alps. Geodin Acta 2: 63–73

5. Blümel P (1983) The western margin of the Bohemian Massif in Bavaria. Fortschr Miner 61: 171–195

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