Geologica Belgica

1374-8505 2034-1954

 

Facteur d'impact : 1.8 (2022)

depuis le 05 février 2011 :
Visualisation(s): 807 (2 ULiège)
Téléchargement(s): 1231 (4 ULiège)
print        
Veerle VANDEGINSTE, Rudy SWENNEN, Jean-Luc Faure, Kirk Osadetz & François ROURE

Paleostress evolution in the Canadian Cordilleran foreland fold-and-thrust belt west of Calgary

(volume 15 (2012) — number 1-2)
Article
Open Access

Document(s) associé(s)

Annexes

Mots-clés : Canada, Cordillera, fault slip data, foreland fold-and-thrust belt, paleostress, stress inversion, tectonic evolution

Abstract

A paleostress analysis was carried out on fault slip data collected at 13 sites distributed over a total of 135 km within the Canadian Rocky Mountains at a latitude of about N51º. Striae on brittle deformation structures were used to calculate paleostress states responsible for the observed deformation, and hence, to unravel the stress state evolution of the Cordilleran foreland fold-and-thrust belt in the study area. We identified five main paleostress states in the study area and interpret these as deformation events in the evolution of the foreland belt. Radial or pure (ENE-WSW) extension and oblique NE-SW to ENE-WSW compression were derived from back-tilted data and were probably active during an early stage. While radial extension may result from increasing burial in the absence of significant horizontal compression, the compression phase may correspond to Middle Jurassic to Late Cretaceous tectonic convergence along the western border of the North American craton. The other three paleostress states include (i) NE-SW to ENE-WSW compression, (ii) compressional NE-SW or pure strike-slip and (iii) pure or strike-slip extension or extensional strike-slip. The NE-SW to ENE-WSW compression and compressional or pure strike-slip phase correspond to the main tectonic compressive stress during Laramide orogeny, consistent with the stress field that caused the macrostructural thrust faults. The final extensional phase may relate to the Eocene regional extensional tectonics.

Pour citer cet article

Veerle VANDEGINSTE, Rudy SWENNEN, Jean-Luc Faure, Kirk Osadetz & François ROURE, «Paleostress evolution in the Canadian Cordilleran foreland fold-and-thrust belt west of Calgary», Geologica Belgica [En ligne], volume 15 (2012), number 1-2, 42-52 URL : https://popups.uliege.be/1374-8505/index.php?id=3505.

A propos de : Veerle VANDEGINSTE

Department of Earth Science and Engineering, South Kensington Campus, Imperial College London, London SW7 2AZ, United Kingdom

A propos de : Rudy SWENNEN

Department of Earth and Environmental Sciences, Section Geology, Katholieke Universiteit Leuven, Celestijnenlaan 200E, B-3001 Heverlee, Belgium

A propos de : Jean-Luc Faure

Institut Français du Pétrole, 1&4 avenue de Bois-Préau, 92852 Rueil-Malmaison Cedex, France

A propos de : Kirk Osadetz

Geological Survey of Canada, 3303 – 33rd Street N.W., Calgary, Alberta

A propos de : François ROURE

Institut Français du Pétrole, 1&4 avenue de Bois-Préau, 92852 Rueil-Malmaison Cedex, France