Twenty million years of continuous deformation along the Karakorum fault, western Tibet: A thermochronological analysis
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Himalayan leucogranites and migmatites: nature, timing and duration of anatexisAcceleration and deceleration of India-Asia convergence since the Cretaceous: Roles of mantle plumes and continental collisionSynkinematic magmatism, heterogeneous deformation, and progressive strain localization in a strike-slip shear zone: The case of the right-lateral Karakorum faultLong-lasting intracontinental strike-slip faulting: new evidence from the Karakorum shear zone in the HimalayasFault weakening across the frictional-viscous transition zone, Karakoram Fault Zone, NW HimalayaEocene Tibetan plateau remnants preserved in the northwest Himalaya
P2860
Twenty million years of continuous deformation along the Karakorum fault, western Tibet: A thermochronological analysis
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article
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wetenschappelijk artikel
@nl
наукова стаття, опублікована в липні 2007
@uk
ലേഖനം
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name
Twenty million years of contin ...... A thermochronological analysis
@en
Twenty million years of contin ...... A thermochronological analysis
@nl
type
label
Twenty million years of contin ...... A thermochronological analysis
@en
Twenty million years of contin ...... A thermochronological analysis
@nl
prefLabel
Twenty million years of contin ...... A thermochronological analysis
@en
Twenty million years of contin ...... A thermochronological analysis
@nl
P2093
P2860
P50
P356
P1433
P1476
Twenty million years of contin ...... A thermochronological analysis
@en
P2093
Edward R. Sobel
Franck Valli
Gweltaz Mahéo
Haibing Li
Nicolas Arnaud
Stéphane Guillot
P2860
P356
10.1029/2005TC001913
P577
2007-07-11T00:00:00Z