Articles | Volume 9, issue 3
https://doi.org/10.5194/se-9-759-2018
© 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-9-759-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
14 Jun 2018
Research article |
| 14 Jun 2018
| 14 Jun 2018
The effect of obliquity on temperature in subduction zones: insights from 3-D numerical modeling
Department of Earth Sciences, Utrecht University, the Netherlands
now at: Sorbonne Université, CNRS-INSU, Institut des Sciences de la Terre Paris, ISTeP UMR 7193, 75005 Paris, France
Cédric Thieulot
Department of Earth Sciences, Utrecht University, the Netherlands
Douwe J. J. van Hinsbergen
Department of Earth Sciences, Utrecht University, the Netherlands
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Cited
24 citations as recorded by crossref.
- Oblique subduction and mantle flow control on upper plate deformation: 3D geodynamic modeling A. Balázs et al. 10.1016/j.epsl.2021.117056
- Geometrical Relations Between Slab Dip and the Location of Volcanic Arcs and Back‐Arc Spreading Centers G. Ha et al. 10.1029/2023GC010997
- Caribbean intra-plate deformation: Paleomagnetic evidence from St. Barthélemy Island for post-Oligocene rotation in the Lesser Antilles forearc M. Philippon et al. 10.1016/j.tecto.2020.228323
- Zircon petrochronology and mineral equilibria of the eclogites from western Tasmania: Interrogating the early Palaeozoic East Gondwana subduction record D. Brown et al. 10.1016/j.gr.2021.02.015
- Exhumation of deeply subducted continental crust along contrasting pathways: Examples from the North Qaidam ultrahigh pressure metamorphic terrane, North Tibet G. Zhou et al. 10.1016/j.gr.2021.11.015
- Geochronology and Zr-in-rutile thermometry of high-pressure/low temperature metamorphic rocks from the Bantimala complex, SW Sulawesi, Indonesia M. Böhnke et al. 10.1016/j.lithos.2018.11.020
- Using 3D kinematic models in subduction channels. The case of the Chañaral tectonic mélange, Coastal Cordillera, northern Chile P. Fuentes et al. 10.1016/j.gr.2018.12.009
- The Geodynamic World Builder: a solution for complex initial conditions in numerical modeling M. Fraters et al. 10.5194/se-10-1785-2019
- Ridge Subduction as a Mechanism for Strike-Slip System Formation: Examples from the Chugach Metamorphic Complex, Alaska, and the Norumbega Fault System, Maine M. Scharman & B. Hooks 10.2139/ssrn.4127317
- Mantle Wedge Seismic Anisotropy and Shear Wave Splitting: Effects of Oblique Subduction L. Kenyon & I. Wada 10.1029/2021JB022752
- Response of a Rheologically Stratified Lithosphere to Subduction of an Indenter‐Shaped Plate: Insights Into Localized Exhumation at Orogen Syntaxes A. Koptev et al. 10.1029/2018TC005455
- Seismicity and mineral destabilizations in the subducting mantle up to 6 GPa, 200 km depth T. Ferrand 10.1016/j.lithos.2019.03.014
- The effect of temperature-dependent material properties on simple thermal models of subduction zones I. van Zelst et al. 10.5194/se-14-683-2023
- Age constraints on high-pressure/low-temperature metamorphism and sedimentation in the Luk Ulo Complex (Java, Indonesia) J. Hoffmann et al. 10.1016/j.lithos.2018.11.019
- Collision Chronology Along the İzmir‐Ankara‐Erzincan Suture Zone: Insights From the Sarıcakaya Basin, Western Anatolia M. Mueller et al. 10.1029/2019TC005683
- Thermal modeling of subduction zones with prescribed and evolving 2D and 3D slab geometries N. Sime et al. 10.1186/s40645-024-00611-4
- On the choice of finite element for applications in geodynamics C. Thieulot & W. Bangerth 10.5194/se-13-229-2022
- An introductory review of the thermal structure of subduction zones: III—Comparison between models and observations P. van Keken & C. Wilson 10.1186/s40645-023-00589-5
- Diachronous demise of the Neotethys Ocean as a driver for non-cylindrical orogenesis in Anatolia D. Gürer & D. van Hinsbergen 10.1016/j.tecto.2018.06.005
- Mafic High‐Pressure Rocks Are Preferentially Exhumed From Warm Subduction Settings P. van Keken et al. 10.1029/2018GC007624
- A simple picture of mantle wedge flow patterns and temperature variation I. Wada 10.1016/j.jog.2021.101848
- Spatio-temporal variability in slab temperature within dynamic 3-D subduction models V. Turino & A. Holt 10.1093/gji/ggad489
- Computing Rates and Distributions of Rock Recovery in Subduction Zones B. Kerswell et al. 10.1029/2022GC010834
- Slab Temperature Evolution Over the Lifetime of a Subduction Zone A. Holt & C. Condit 10.1029/2020GC009476
24 citations as recorded by crossref.
- Oblique subduction and mantle flow control on upper plate deformation: 3D geodynamic modeling A. Balázs et al. 10.1016/j.epsl.2021.117056
- Geometrical Relations Between Slab Dip and the Location of Volcanic Arcs and Back‐Arc Spreading Centers G. Ha et al. 10.1029/2023GC010997
- Caribbean intra-plate deformation: Paleomagnetic evidence from St. Barthélemy Island for post-Oligocene rotation in the Lesser Antilles forearc M. Philippon et al. 10.1016/j.tecto.2020.228323
- Zircon petrochronology and mineral equilibria of the eclogites from western Tasmania: Interrogating the early Palaeozoic East Gondwana subduction record D. Brown et al. 10.1016/j.gr.2021.02.015
- Exhumation of deeply subducted continental crust along contrasting pathways: Examples from the North Qaidam ultrahigh pressure metamorphic terrane, North Tibet G. Zhou et al. 10.1016/j.gr.2021.11.015
- Geochronology and Zr-in-rutile thermometry of high-pressure/low temperature metamorphic rocks from the Bantimala complex, SW Sulawesi, Indonesia M. Böhnke et al. 10.1016/j.lithos.2018.11.020
- Using 3D kinematic models in subduction channels. The case of the Chañaral tectonic mélange, Coastal Cordillera, northern Chile P. Fuentes et al. 10.1016/j.gr.2018.12.009
- The Geodynamic World Builder: a solution for complex initial conditions in numerical modeling M. Fraters et al. 10.5194/se-10-1785-2019
- Ridge Subduction as a Mechanism for Strike-Slip System Formation: Examples from the Chugach Metamorphic Complex, Alaska, and the Norumbega Fault System, Maine M. Scharman & B. Hooks 10.2139/ssrn.4127317
- Mantle Wedge Seismic Anisotropy and Shear Wave Splitting: Effects of Oblique Subduction L. Kenyon & I. Wada 10.1029/2021JB022752
- Response of a Rheologically Stratified Lithosphere to Subduction of an Indenter‐Shaped Plate: Insights Into Localized Exhumation at Orogen Syntaxes A. Koptev et al. 10.1029/2018TC005455
- Seismicity and mineral destabilizations in the subducting mantle up to 6 GPa, 200 km depth T. Ferrand 10.1016/j.lithos.2019.03.014
- The effect of temperature-dependent material properties on simple thermal models of subduction zones I. van Zelst et al. 10.5194/se-14-683-2023
- Age constraints on high-pressure/low-temperature metamorphism and sedimentation in the Luk Ulo Complex (Java, Indonesia) J. Hoffmann et al. 10.1016/j.lithos.2018.11.019
- Collision Chronology Along the İzmir‐Ankara‐Erzincan Suture Zone: Insights From the Sarıcakaya Basin, Western Anatolia M. Mueller et al. 10.1029/2019TC005683
- Thermal modeling of subduction zones with prescribed and evolving 2D and 3D slab geometries N. Sime et al. 10.1186/s40645-024-00611-4
- On the choice of finite element for applications in geodynamics C. Thieulot & W. Bangerth 10.5194/se-13-229-2022
- An introductory review of the thermal structure of subduction zones: III—Comparison between models and observations P. van Keken & C. Wilson 10.1186/s40645-023-00589-5
- Diachronous demise of the Neotethys Ocean as a driver for non-cylindrical orogenesis in Anatolia D. Gürer & D. van Hinsbergen 10.1016/j.tecto.2018.06.005
- Mafic High‐Pressure Rocks Are Preferentially Exhumed From Warm Subduction Settings P. van Keken et al. 10.1029/2018GC007624
- A simple picture of mantle wedge flow patterns and temperature variation I. Wada 10.1016/j.jog.2021.101848
- Spatio-temporal variability in slab temperature within dynamic 3-D subduction models V. Turino & A. Holt 10.1093/gji/ggad489
- Computing Rates and Distributions of Rock Recovery in Subduction Zones B. Kerswell et al. 10.1029/2022GC010834
- Slab Temperature Evolution Over the Lifetime of a Subduction Zone A. Holt & C. Condit 10.1029/2020GC009476
Discussed (final revised paper)
Latest update: 18 Apr 2024
Short summary
The thermal state of the Earth's crust determines how it reacts to tectonic forces and to fluid flow responsible for ore formation. We hypothesize that the angle between plate motion and convergent boundaries determines the thermal regime of subduction zones (where a plate goes under another one). Computer models and a geological reconstruction of Turkey were used to validate this hypothesis.
This research was done to validate a hypothesis made on the basis of nonquantitative field data.
The thermal state of the Earth's crust determines how it reacts to tectonic forces and to fluid...
