Linking deep and shallow crustal processes during regional transtension in an exhumed continental arc, north Cascades, northwestern Cordillera (USA)

The North Cascades orogen (northwestern USA) provides an exceptional natural laboratory with which to evaluate potential temporal and kinematic links between processes operating at a wide range of crustal levels during collapse of a continental arc, and particularly the compatibility of strain betwe...

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Veröffentlicht in:	Geosphere (Boulder, Colo.) Colo.), 2016-06, Vol.12 (3), p.900-924
Hauptverfasser:	Miller, Robert B, Gordon, Stacia M, Bowring, Samuel, Doran, Brigid, McLean, Noah, Michels, Zachary, Shea, Erin, Whitney, Donna L
Format:	Artikel
Sprache:	eng
Schlagworte:	absolute age Basins British Columbia brittle deformation Canada Cascade Range Cascades Cenozoic Collapse Compatibility cross sections crust Crusts dates deformation Dikes ductile deformation Eocene exhumation faults Geophysics Gneiss gneisses igneous and metamorphic rocks intrusions island arcs lower crust metamorphic core complexes metamorphic rocks metamorphism migmatization nesosilicates North America North American Cordillera northern Cascade Range orthogneiss orthosilicates P-T conditions Paleogene Petrology plate collision plate tectonics plutons silicates Skagit Gneiss solid Earth (tectonophysics) southwestern British Columbia Strain Swakane Gneiss tectonics Tertiary transtension U/Pb United States upper crust Washington Western Canada zircon zircon group
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