Physics
Scientific paper
Aug 2005
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2005e%26psl.236..814v&link_type=abstract
Earth and Planetary Science Letters, Volume 236, Issue 3-4, p. 814-827.
Physics
5
Scientific paper
The flat surface of orogenic plateaus requires a weak detachment at the base of the crust that prevents the formation of large-wavelength topography in the centre of the orogen and decouples the deformation of crust and mantle. This study uses numerical distinct-element simulations of plateau orogeny to show that the mass flux across the lateral tips of this detachment controls the shape and kinematics of the plateau flanks. If the mass flux is directed towards the plateau, e.g. foreland crust moves into the detached section, it forms a low-slope, small-taper pro-flank. If the mass flux is directed outward, thrusting towards the foreland generates a steep-slope, large-taper retro-flank. The mass flux itself is controlled by the shear strength distribution at the base of the crust. The two general types of orogenic flanks from three combinations that can be used to classify the evolution of plateau orogens in general. Application of this concept to the Andes allows to decode the lower crustal shear strength distribution during the formation of the Altiplano Puna plateau. Their western slope is a retro-flank localized by the underlying oceanic subduction zone. On the eastern side a pro-flank accretes foreland crust, which is progressively decoupled from the moving mantle below.
Oncken Onno
Vietor Tim
No associations
LandOfFree
Controls on the shape and kinematics of the Central Andean plateau flanks: Insights from numerical modeling does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.
If you have personal experience with Controls on the shape and kinematics of the Central Andean plateau flanks: Insights from numerical modeling, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Controls on the shape and kinematics of the Central Andean plateau flanks: Insights from numerical modeling will most certainly appreciate the feedback.
Profile ID: LFWR-SCP-O-953318