T246 Challenges in Tectonics: Dynamic Interactions among Earth-Surface Processes, Landscape Evolution, and Tectonics II

Tuesday, 24 October 2017
1:30 PM - 5:30 PM
Tahoma 4

ALL SMEARED? GEOMORPHIC RESPONSES TO HORIZONTAL MOVEMENT AT GEOLOGIC TIME SCALES

Paper number: T246-12
Program: Technical Sessions
Time: 4:25 PM – 4:40 PM

Authors

Abstract

Landscapes represent the interaction between surface processes, rock properties, and tectonic deformation. In active fold-thrust belts rock uplift is controlled by the geometry of the detachment fault, specifically, the location and angle of fault ramps. These ramps are associated with high topography, significant relief and steep river channels. However, such rock uplift is more complex in that it comprises both vertical and horizontal components of displacement, and thus raises the question whether geomorphic markers of uplift can be laterally displaced. In the hinterland of the Himalaya, where high erosion rates accompany high convergence rates of ~ 20 mm/yr, normalized channel steepness (ksn) values increase to the north over ~ 25 km with the highest values marking the proposed location of the active ramp. Similarly, in the Andes, where low erosion rates attend low convergence rates of ~ 5-10 mm/yr, ksn values increase westward over ~ 40 km. These ksn values that decrease in the direction of movement may indicate decreasing uplift, or may be a function of horizontal displacement. The question arises, how the relationship between convergence rates, rock erodibility and thrust ramp geometry might affect topography, relief, and ksn values. In this study, we explore the displacement of ksn values (i) analytically, by quantifying ksn migration in 1D through a ratio of erodibility over convergence rate, and (ii) numerically by integrating realistic displacement kinematics with the Cascade landscape evolution algorithm in 3D. Our results indicate that a horizontal movement component causes an asymmetry in topography and relief, and a smearing of ksn in the direction of movement away from the vertical uplift field. The extent of this shift is dependent on the ratio of erodibility over convergence rate for a given structural geometry. As this ratio decreases, such that convergence rates are significantly higher than erosion (~ 5-10 times), the smearing can extend to tens of km from the ramp front. Sets of parameters that are representative for the hinterland of the Himalaya and the Andes have low erodibility to convergence ratios such that ksn values are smeared over such a distance. Thus, we argue that the interpretation of geomorphic markers at convergent orogens requires consideration of horizontal displacement.

Geological Society of America Abstracts with Programs. Vol. 49, No. 6

doi: 10.1130/abs/2017AM-301226

© Copyright 2017 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.