Crustal-scale fluid flow during the tectonic evolution of the Bighorn Basin (Wyoming, USA)

Author:

Beaudoin Nicolas12,Bellahsen Nicolas12,Lacombe Olivier12,Emmanuel Laurent12,Pironon Jacques3

Affiliation:

1. UPMC Univ Paris 06; UMR 7193; ISTEP; F-75005 Paris France

2. CNRS; UMR 7193; ISTEP; F-75005 Paris France

3. Université; de Loraine; CNRS, CREGU, UMR 7359 Geo Resources, BP 70239; F-54506 Vandoeuvre-lés, Nancy Cedex France

Publisher

Wiley

Subject

Geology

Reference130 articles.

1. Evidence for pre-folding vein development in the Oligo-Miocene Asmari Formation in the Central Zagros Fold Belt, Iran;Ahmadhadi;Tectonics,2008

2. Stress and strain patterns, kinematics and deformation mechanisms in a basement-cored anticline: Sheep Mountain Anticline, Wyoming;Amrouch;Tectonics,2010

3. Paleostress magnitudes in folded sedimentary rocks;Amrouch;Geophys. Res. Lett.,2011

4. Evolution of synorogenic clastic deposits in the intermontane Uinta Basin of Utah;Anderson;SEPM Spec. Publ.,1974

5. Andrews , D.A. Pierce , W.G. Eargle , D.H. 1947 Geological map of the Bighorn Basin, Wyoming and Montana

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