Thrust-related, diapiric, and extensional doming in a frontal orogenic wedge: example of the Montagne Noire, Southern French Hercynian Belt

Author:

Soula Jean-Claude,Debat Pierre,Brusset Stéphane,Bessière Gilbert,Christophoul Frédéric,Déramond Joachim

Publisher

Elsevier BV

Subject

Geology

Reference145 articles.

1. Tectonic evolution of the Montagne Noire and a possible orogenic model for syncollisional exhumation of deep rocks, Variscan belt, France;Aerden;Tectonics,1998

2. Origin of a large-scale fold nappe in the Montagne Noire, Variscan belt, France;Aerden;Journal of Structural Geology,1999

3. Cenozoic and Mesozoic structure of the eastern Basin and Range Province, Utah, from COCORP seismic reflection data;Allmendinger;Geology,1983

4. The cordierite–garnet–sillimanite–quartz equilibrium: experiments and applications;Aranovich,1983

5. Arthaud, F., 1970. Etude tectonique et microtectonique comparée de deux domaines hercyniens: les nappes de la Montagne Noire (France) et l'anticlinorium de l'Iglesiente (Sardaigne). Thesis, University of Montpellier.

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