Fracture-controlled paleohydrogeology in a basement-cored, fault-related fold: Sheep Mountain Anticline, Wyoming, United States
Author:
Affiliation:
1. ISTEP, UMR 7193; UPMC Université de Paris 6, CNRS; F-75005; Paris; France
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.agu.org/journals/gc/gc1106/2010GC003494/2010GC003494.pdf
Reference57 articles.
1. Stress and strain patterns, kinematics and deformation mechanisms in a basement-cored anticline: Sheep Mountain Anticline, Wyoming;Amrouch;Tectonics,2010
2. Constraints on deformation mechanisms during folding provided by rock physical properties: A case study at Sheep Mountain anticline (Wyoming, USA);Amrouch;Geophys. J. Int.,2010
3. Depositional history of the Cambrian Flathead Standstone, Park County, Wyoming;Bell;Wyo. Geol. Assoc. Guideb.,1970
4. The role of fractures in the structural interpretation of Sheep Mountain Anticline, Wyoming;Bellahsen;J. Struct. Geol.,2006
5. The role of fractures in the structural interpretation of Sheep Mountain Anticline, Wyoming;Bellahsen;J. Struct. Geol.,2006
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