Development of a synorogenic composite sill at deep structural levels of a magmatic arc (Odenwald, Germany). Part 2: Rheological inversion and mullion formation under bulk constriction-Reference-Cited by-同舟云学术

Development of a synorogenic composite sill at deep structural levels of a magmatic arc (Odenwald, Germany). Part 2: Rheological inversion and mullion formation under bulk constriction

Published:2022-02 Issue: Volume:155 Page:104525
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Zulauf G.,Zulauf J.,Linckens J.,Gerdes A.,Hattingen E.,Loeckle F.,Marschall H.R.,Steckenreiter L.

Publisher

Elsevier BV

Subject

Geology

Reference95 articles.

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3. Plutonism in the variscan Odenwald (Germany): from subduction to collision;Altherr;Int. J. Earth Sci.,1999

4. Deformation mechanisms and reaction of hornblende: examples from the Bergell tonalite (Central Alps);Berger;Tectonophysics,1996

5. C-slip in quartz from subsolidus deformed granite;Blumenfeld;Tectonophysics,1986

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