Dynamic interactions between erosion, deposition, and three‐dimensional deformation in compressional fold belt settings
G Simpson - Journal of Geophysical Research: Earth Surface, 2004 - Wiley Online Library
This study investigates whether the three‐dimensionality of erosion and deposition can
influence three‐dimensional folding, even when compression is purely convergent. This …
influence three‐dimensional folding, even when compression is purely convergent. This …
A dynamic model to investigate coupling between erosion, deposition, and three‐dimensional (thin‐plate) deformation
G Simpson - Journal of Geophysical Research: Earth Surface, 2004 - Wiley Online Library
This paper presents a mathematical model developed to investigate fully coupled
interactions between erosion, deposition, and dynamic three‐dimensional deformation …
interactions between erosion, deposition, and dynamic three‐dimensional deformation …
River transport effects on compressional belts: First results from an integrated analogue‐numerical model
KS Persson, D Garcia‐Castellanos… - Journal of Geophysical …, 2004 - Wiley Online Library
Erosion, deposition, and tectonic processes interact to define the style of deformation in
compressional belts. This paper introduces a method of integrating a numerical model for …
compressional belts. This paper introduces a method of integrating a numerical model for …
Tectonic geomorphology of active folding and development of transverse drainages
EA Keller, DE DeVecchio - Treatise on Geomorphology …, 2013 - asu.elsevierpure.com
Two fundamental geomorphic questions are:(1) Do growing folds propagate laterally? and
(2) how does transverse drainage develop across an active fold belt? Research during the …
(2) how does transverse drainage develop across an active fold belt? Research during the …
Influences of surface processes on fold growth during 3‐D detachment folding
In order to understand the interactions between surface processes and multilayer folding
systems, we here present fully coupled three‐dimensional numerical simulations. The …
systems, we here present fully coupled three‐dimensional numerical simulations. The …
[HTML][HTML] Three-dimensional growth of flexural slip fault-bend and fault-propagation folds and their geomorphic expression
A Bernal, S Hardy, RL Gawthorpe - Geosciences, 2018 - mdpi.com
The three-dimensional growth of fault-related folds is known to be an important process
during the development of compressive mountain belts. However, comparatively little is …
during the development of compressive mountain belts. However, comparatively little is …
Geometric and numerical model of progressive limb rotation in detachment folds
A simple, area-balanced, geometric model of progressive limb rotation in detachment folds
allows the quantification of displacement, uplift, and rotation and the assessment of their …
allows the quantification of displacement, uplift, and rotation and the assessment of their …
Erosional dynamics, flexural isostasy, and long‐lived escarpments: A numerical modeling study
GE Tucker, RL Slingerland - Journal of Geophysical Research …, 1994 - Wiley Online Library
Erosional escarpments are common features of high‐elevation rifted continents. Fission
track data suggest that these escarpments form by base level lowering and/or marginal uplift …
track data suggest that these escarpments form by base level lowering and/or marginal uplift …
Kinematic implications of consequent channels on growing folds
JK Goode, DW Burbank - Journal of Geophysical Research …, 2011 - Wiley Online Library
As soon as a fold begins to grow above base level, it becomes subject to erosion. A
numerical model of simultaneous fold growth and river erosion captures the early stages of …
numerical model of simultaneous fold growth and river erosion captures the early stages of …
Influence of erosion and deposition on deformation in fold belts
G Simpson - 2006 - pubs.geoscienceworld.org
This paper investigates whether surface processes such as erosion and deposition have
any influence on folding of the upper crust at small to intermediate spatial scales (ie,< 200 …
any influence on folding of the upper crust at small to intermediate spatial scales (ie,< 200 …