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Geological Society, London, Special Publications; 2005; v. 245; p. 39-64;
DOI: 10.1144/GSL.SP.2005.245.01.03
© 2005 Geological Society of London

Flow of partially molten crust and origin of detachments during collapse of the Cordilleran Orogen

C. Teyssier1, E. C. Ferré2, D. L. Whitney1, B. Norlander1, O. Vanderhaeghe3 & D. Parkinson4,5

1 Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA
2 Department of Geology, Southern Illinois University, Mailcode 4324, Carbondale, IL 62901, USA
3 Université de Nancy 1, UMR 7566 G2R, BP 239, 54506 Vandoeuvre-les-Nancy, France
4 Department of Geological Sciences, University of California, Santa Barbara, CA 93106, USA
5 , 429 N 190th Street, Seattle, WA 98133, USA

In metamorphic core complexes two types of detachments develop, coupled by flow of partially molten crust: a channel detachment and a rolling-hinge detachment. The channel detachment, on the hinterland side of the orogen, represents the long-lived interface that separates the partially molten crust flowing in a channel from the rigid upper crustal lid. On the foreland side of the core complex, a rolling-hinge detachment develops. This detachment dips toward the foreland, probably affects the whole crust, and its geometry is governed by strain localization at the critical interface between cold foreland and hot hinterland. Activation of the rolling-hinge detachment drives rapid decompression and melting, leading to the diapiric rise of migmatite domes in the footwall of the detachment. A kinematic hinge (switch in sense of shear) separates the two types of detachments. Structural, metamorphic and geo/thermochronological studies in the Shuswap core complex (North American Cordillera), combined with an anisotropy of magnetic susceptibility study of leucogranites concentrated in the detachments, suggest that this orogen collapsed rapidly through the development of channel and rolling-hinge detachments in the early Eocene. The kinematic hinge is currently located approximately 40 km west of the footwall in which it originated, corresponding to a mean exhumation rate of >5 km Ma–1, which explains the near-isothermal decompression recorded within the migmatite dome.





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