Download presentation
Presentation is loading. Please wait.
Published byMyron McGee Modified over 9 years ago
1
Sevier- and Laramide-Style Tectonics in the Northern Rocky Mountains John S. Oldow Geological Sciences University of Idaho Moscow, Idaho
2
Tectonic Transition between northern and southern Cordillera McClelland and Oldow, 2005
3
Scientific Motivation 1. 3 dimensional architecture of contractional orogen 2. Degree of coupling between crust and mantle during plate boundary deformation 3. Plate margin modification during terrane accretion 4. Role of structural inheritance
4
Western margin of Mesozoic continental crust
5
Jurassic magmatic arc
6
Jurassic backarc deformation
7
Late Jurassic accretion of Wallowa terrane
8
Late Jurassic-Early Cretaceous backarc basin transpression
9
Late Jurassic and Cretaceous foreland thrusting
37
Research Opportunities 1.Transition from thin-skinned to thick-skinned foreland contraction 2. Displacement transfer from foreland contraction to hinterland crustal duplex 3.Plate boundary modification during terrane accretion 4.Role of structural inheritance in continental tectonics
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.