Articles | Volume 9, issue 6
https://doi.org/10.5194/se-9-1207-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-9-1207-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
05 Nov 2018
Research article | Highlight paper |
| 05 Nov 2018
| 05 Nov 2018
The influence of upper-plate advance and erosion on overriding plate deformation in orogen syntaxes
Matthias Nettesheim
Department of Geology, University of Tübingen, Tübingen, Germany
Todd A. Ehlers
CORRESPONDING AUTHOR
Department of Geology, University of Tübingen, Tübingen, Germany
David M. Whipp
Department of Geosciences and Geography, University of Helsinki, Helsinki, Finland
Alexander Koptev
Department of Geology, University of Tübingen, Tübingen, Germany
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Cited
23 citations as recorded by crossref.
- Numerical modelling of coupled climate, tectonics, and surface processes on the eastern Himalayan syntaxis X. Lu et al.
- Uplift, tilting, and underlying structures of coastal northwestern Luzon, Philippines, deduced from marine terraces Y. Wang et al.
- Coupled surface to deep Earth processes: Perspectives from TOPO-EUROPE with an emphasis on climate- and energy-related societal challenges S. Cloetingh et al.
- The role of continental lithospheric thermal structure in the evolution of orogenic systems: application to the Himalayan–Tibetan collision zone M. Liu et al.
- How do pre-existing weak zones and rheological layering of the continental lithosphere influence the development and evolution of intra-continental subduction? M. Liu & D. Yang
- Effects of Along‐Trench Asymmetric Subduction Initiation on Plate Rotation and Trench Migration: A Laboratory Modeling Perspective C. Wang et al.
- Connection Between a Subcontinental Plume and the Mid‐Lithospheric Discontinuity Leads to Fast and Intense Craton Lithospheric Thinning Y. Shi et al.
- Opposite rotations in the Central Andes Bend: Tectonic scenario compared to other cases of opposite rotations and implications for long-term subduction at continental arcs A. Martin
- Using benthic foraminifera as bioindicators of environmental change in coastal lagoons P. Belart et al.
- Response of a Rheologically Stratified Lithosphere to Subduction of an Indenter‐Shaped Plate: Insights Into Localized Exhumation at Orogen Syntaxes A. Koptev et al.
- Development of surface ruptures by hanging-wall extension over a thrust ramp along the Ragged Mountain fault, Katalla, Alaska, USA: Applications of high-resolution three-dimensional terrain models S. Heinlein et al.
- 3D geodynamic-geomorphologic modelling of deformation and exhumation at curved plate boundaries: Implications for the southern Alaskan plate corner A. Koptev et al.
- Multi-stage tectonic events of the Eastern Kunlun Mountains, Northern Tibetan Plateau constrained by fission track thermochronology P. Tian et al.
- On the criticality of return flows in viscous accretionary wedges and its implications for deep-crustal exhumation in subduction zones A. Patsa & N. Mandal
- Transitions in subduction zone properties align with long-term topographic growth (Cascadia, USA) L. Michel-Wolf et al.
- Plume‐Induced Sinking of Intracontinental Lithospheric Mantle: An Overlooked Mechanism of Subduction Initiation? S. Cloetingh et al.
- Subduction development along extinct mid-ocean ridges versus weakened passive continental margins Y. Wu et al.
- Architecture and kinematics of the Famatinian deformation in the Sierra Grande de San Luis: A record of a collisional history at 33° S latitude A. Morosini et al.
- Slab Subduction and Pull Link Magmatism at Active and Passive Continental Margins L. Dai et al.
- Bias and error in modelling thermochronometric data: resolving a potential increase in Plio-Pleistocene erosion rate S. Willett et al.
- Plate corner subduction and rapid localized exhumation: Insights from3Dcoupled geodynamic and geomorphological modelling A. Koptev et al.
- Control of slab tears and slab flat wedging on volcanism in the Alaska subduction zone Y. Hu et al.
- Understanding subduction infancy to mature subduction in Southwest Japan via the self-consistent formation of a weak slab interface C. Lee & Y. Kim
23 citations as recorded by crossref.
- Numerical modelling of coupled climate, tectonics, and surface processes on the eastern Himalayan syntaxis X. Lu et al.
- Uplift, tilting, and underlying structures of coastal northwestern Luzon, Philippines, deduced from marine terraces Y. Wang et al.
- Coupled surface to deep Earth processes: Perspectives from TOPO-EUROPE with an emphasis on climate- and energy-related societal challenges S. Cloetingh et al.
- The role of continental lithospheric thermal structure in the evolution of orogenic systems: application to the Himalayan–Tibetan collision zone M. Liu et al.
- How do pre-existing weak zones and rheological layering of the continental lithosphere influence the development and evolution of intra-continental subduction? M. Liu & D. Yang
- Effects of Along‐Trench Asymmetric Subduction Initiation on Plate Rotation and Trench Migration: A Laboratory Modeling Perspective C. Wang et al.
- Connection Between a Subcontinental Plume and the Mid‐Lithospheric Discontinuity Leads to Fast and Intense Craton Lithospheric Thinning Y. Shi et al.
- Opposite rotations in the Central Andes Bend: Tectonic scenario compared to other cases of opposite rotations and implications for long-term subduction at continental arcs A. Martin
- Using benthic foraminifera as bioindicators of environmental change in coastal lagoons P. Belart et al.
- Response of a Rheologically Stratified Lithosphere to Subduction of an Indenter‐Shaped Plate: Insights Into Localized Exhumation at Orogen Syntaxes A. Koptev et al.
- Development of surface ruptures by hanging-wall extension over a thrust ramp along the Ragged Mountain fault, Katalla, Alaska, USA: Applications of high-resolution three-dimensional terrain models S. Heinlein et al.
- 3D geodynamic-geomorphologic modelling of deformation and exhumation at curved plate boundaries: Implications for the southern Alaskan plate corner A. Koptev et al.
- Multi-stage tectonic events of the Eastern Kunlun Mountains, Northern Tibetan Plateau constrained by fission track thermochronology P. Tian et al.
- On the criticality of return flows in viscous accretionary wedges and its implications for deep-crustal exhumation in subduction zones A. Patsa & N. Mandal
- Transitions in subduction zone properties align with long-term topographic growth (Cascadia, USA) L. Michel-Wolf et al.
- Plume‐Induced Sinking of Intracontinental Lithospheric Mantle: An Overlooked Mechanism of Subduction Initiation? S. Cloetingh et al.
- Subduction development along extinct mid-ocean ridges versus weakened passive continental margins Y. Wu et al.
- Architecture and kinematics of the Famatinian deformation in the Sierra Grande de San Luis: A record of a collisional history at 33° S latitude A. Morosini et al.
- Slab Subduction and Pull Link Magmatism at Active and Passive Continental Margins L. Dai et al.
- Bias and error in modelling thermochronometric data: resolving a potential increase in Plio-Pleistocene erosion rate S. Willett et al.
- Plate corner subduction and rapid localized exhumation: Insights from3Dcoupled geodynamic and geomorphological modelling A. Koptev et al.
- Control of slab tears and slab flat wedging on volcanism in the Alaska subduction zone Y. Hu et al.
- Understanding subduction infancy to mature subduction in Southwest Japan via the self-consistent formation of a weak slab interface C. Lee & Y. Kim
Saved (final revised paper)
Latest update: 30 Apr 2026
Short summary
In this modeling study, we investigate rock uplift at plate corners (syntaxes). These are characterized by a unique bent geometry at subduction zones and exhibit some of the world's highest rock uplift rates. We find that the style of deformation changes above the plate's bent section and that active subduction is necessary to generate an isolated region of rapid uplift. Strong erosion there localizes uplift on even smaller scales, suggesting both tectonic and surface processes are important.
In this modeling study, we investigate rock uplift at plate corners (syntaxes). These are...
