Stress and strain patterns, kinematics and deformation mechanisms in a basement-cored anticline: Sheep Mountain Anticline, Wyoming
Author:
Affiliation:
1. ISTEP, UMR 7193; Université Pierre et Marie Curie, CNRS; Paris; France
2. Division Géologie-Géochimie-Géophysique; Institut Français du Pétrole; Rueil-Malmaison; France
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.agu.org/journals/tc/tc1001/2009TC002525/2009TC002525.pdf
Reference109 articles.
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2. Inversion of field data in fault tectonics to obtain the regional stress. III: A new rapid direct inversion method by analytical means;Angelier;Geophys. J. Int.,1990
3. Beaudoin , N. 2009 Étude géochimique et microstructurale de la fracturation de Sheep Mountain Anticline: Mise en évidence de paléocirculations de fluides et implications structurales Univ. Paris 6 Paris
4. The role of fractures in the structural interpretation of Sheep Mountain Anticline, Wyoming;Bellahsen;J. Struct. Geol.,2006
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