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Funder Unable to find ROR for Asociación Colombiana de Geólogos y Geofísicos del Petróleo Unable to find ROR for Australian Research Council Model code URI/DOI Warning: No URI/DOI provided. Model output URI/DOI Warning: No URI/DOI provided. Computer URI/DOI Warning: No URI/DOI provided. Animation Warning: No animation uploaded.
Model setup figure Error: No caption found for image.
Creator/Contributor Creator/contributor is Andres Felipe Rodriguez Corcho (0000-0002-1521-7910)
Model Repository Slug
Model repo will be created with name corcho_2022_collision
Field of Research (FoR) Codes
#FoR_370604
: Geodynamics License MIT License
Model Category
Associated Publication Found publication: The Role of Lithospheric‐Deep Mantle Interactions on the Style and Stress Evolution of Arc‐Continent Collision
Title The Role of Lithospheric‐Deep Mantle Interactions on the Style and Stress Evolution of Arc‐Continent Collision
Description We investigate how the mechanical properties of intra‐oceanic arcs affect the collision style and associated stress‐strain evolution with buoyancy‐driven models of subduction that accurately reproduce the dynamic interaction of the lithosphere and mantle. We performed a series of simulations only varying the effective arc thickness as it controls the buoyancy of intra‐oceanic arcs. Our simulations spontaneously evolve into two contrasting styles of collision that are controlled by a 3% density contrast between the arc and the continental plate. In simulations with less buoyant arcs (15–31 km; effective thickness), we observe arc‐transference to the overriding plate and slab‐anchoring and folding at the 660 km transition zone that result in fluctuations in the slab dip, strain‐stress regime, surface kinematics, and viscous dissipation. After slab‐folding occurs, the gravitational potential energy is dissipated in the form of lithospheric flow causing lithospheric extension in the overriding plate. Conversely, simulations with more buoyant arcs (32–35 km; effective thickness) do not lead to arc‐transference and result in slab break‐off, which causes an asymptotic trend in surface kinematics, viscous dissipation and strain‐stress regime, and lithospheric extension in the overriding plate. The results of our numerical modeling highlight the importance of slab‐anchoring and folding in the 660 km transition zone on increasing the mechanical coupling of the subduction system.
Model Authors
Scientific Keywords
Funder
Include model code? True
Include model output data? True
Software Framework DOI/URI Found software: UWGeodynamics: A teaching an research tool for numerical geodynamic modelling
Software Repository https://github.com/underworldcode/UWGeodynamics
Name of primary software framework UWGeodynamics: A teaching an research tool for numerical geodynamic modelling
Software framework authors
Software & algorithm keywords
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Graphic abstract Filename: graphic_abstract.png Caption: Here is a caption for the image written on a separate line above the image link.
Model setup figure Filename: model_setup.jpg Caption:
Model setup description Here is a description of the model setup. Here is a description of the model setup. Here is a description of the model setup
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We performed a series of simulations only varying the effective arc thickness as it controls the buoyancy of intra‐oceanic arcs. Our simulations spontaneously evolve into two contrasting styles of collision that are controlled by a 3% density contrast between the arc and the continental plate. In simulations with less buoyant arcs (15–31\xa0km; effective thickness), we observe arc‐transference to the overriding plate and slab‐anchoring and folding at the 660\xa0km transition zone that result in fluctuations in the slab dip, strain‐stress regime, surface kinematics, and viscous dissipation. After slab‐folding occurs, the gravitational potential energy is dissipated in the form of lithospheric flow causing lithospheric extension in the overriding plate. Conversely, simulations with more buoyant arcs (32–35\xa0km; effective thickness) do not lead to arc‐transference and result in slab break‐off, which causes an asymptotic trend in surface kinematics, viscous dissipation and strain‐stress regime, and lithospheric extension in the overriding plate. The results of our numerical modeling highlight the importance of slab‐anchoring and folding in the 660\xa0km transition zone on increasing the mechanical coupling of the subduction system.', 'identifier': ['10.1029/2022GC010386'], 'funder': [{'@type': 'Organization', 'name': 'University of Melbourne'}]}, 'title': 'The Role of Lithospheric‐Deep Mantle Interactions on the Style and Stress Evolution of Arc‐Continent Collision', 'description': 'We investigate how the mechanical properties of intra‐oceanic arcs affect the collision style and associated stress‐strain evolution with buoyancy‐driven models of subduction that accurately reproduce the dynamic interaction of the lithosphere and mantle. We performed a series of simulations only varying the effective arc thickness as it controls the buoyancy of intra‐oceanic arcs. Our simulations spontaneously evolve into two contrasting styles of collision that are controlled by a 3% density contrast between the arc and the continental plate. In simulations with less buoyant arcs (15–31\xa0km; effective thickness), we observe arc‐transference to the overriding plate and slab‐anchoring and folding at the 660\xa0km transition zone that result in fluctuations in the slab dip, strain‐stress regime, surface kinematics, and viscous dissipation. After slab‐folding occurs, the gravitational potential energy is dissipated in the form of lithospheric flow causing lithospheric extension in the overriding plate. 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The results of our numerical modeling highlight the importance of slab‐anchoring and folding in the 660\xa0km transition zone on increasing the mechanical coupling of the subduction system.', 'authors': [{'@type': 'Person', '@id': 'http://orcid.org/0000-0002-1521-7910', 'givenName': 'Andrés Felipe', 'familyName': 'Rodríguez Corcho', 'affiliation': [{'@type': 'Organization', 'name': 'School of Geography, Earth and Atmospheric Sciences University of Melbourne Melbourne VIC Australia'}, {'@type': 'Organization', 'name': 'School of Geosciences University of Sydney Sydney NSW Australia'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0002-1270-4377', 'givenName': 'Sara', 'familyName': 'Polanco', 'affiliation': [{'@type': 'Organization', 'name': 'School of Geosciences University of Sydney Sydney NSW Australia'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0002-2594-6965', 'givenName': 'Rebecca', 'familyName': 'Farrington', 'affiliation': [{'@type': 'Organization', 'name': 'School of Geography, Earth and Atmospheric Sciences University of Melbourne Melbourne VIC Australia'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0003-3891-5444', 'givenName': 'Romain', 'familyName': 'Beucher', 'affiliation': [{'@type': 'Organization', 'name': 'Research School of Earth Sciences Australian National University Canberra ACT Australia'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0002-3553-0787', 'givenName': 'Camilo', 'familyName': 'Montes', 'affiliation': [{'@type': 'Organization', 'name': 'Department of Physics and Geosciences Universidad del Norte Barranquilla Colombia'}]}, {'@type': 'Person', '@id': 'http://orcid.org/0000-0003-3685-174X', 'givenName': 'Louis', 'familyName': 'Moresi', 'affiliation': [{'@type': 'Organization', 'name': 'Research School of Earth Sciences Australian National University Canberra ACT Australia'}]}], 'keywords': ['Subduction', 'collision', 'arcs'], 'funder': [{'@type': 'Organization', 'name': 'Asociación Colombiana de Geólogos y Geofísicos del Petróleo', 'url': 'Asociación Colombiana de Geólogos y Geofísicos del Petróleo'}, {'@type': 'Organization', 'name': 'Australian Research Council', 'url': 'Australian Research Council'}], 'include_model_code': True, 'include_model_output': True, 'software': {'@type': 'SoftwareApplication', '@id': 'https://doi.org/10.5281/zenodo.5606117', 'name': 'UWGeodynamics: A teaching an research tool for numerical geodynamic modelling', 'softwareVersion': 'v2.11.0', 'author': [{'@type': 'Person', '@id': '0000-0003-3891-5444', 'name': 'Romain Beucher', 'affiliation': 'School of Earth Science, The University of Melbourne'}, {'@type': 'Person', '@id': '0000-0003-3685-174X', 'name': 'Louis Moresi', 'affiliation': 'Research School of Earth Sciences, The Australian National University; 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Model repository created at https://github.com/hvidy/corcho_2022_collision
-> creator/contributor ORCID (or name)
0000-0002-1521-7910
-> slug
corcho_2022_collision
-> field of Research (FoR) Codes
370604
-> license
MIT
-> model category
model published in study
-> associated publication DOI
http://dx.doi.org/10.1029/2022gc010386
-> title
No response
-> description
No response
-> model authors
No response
-> scientific keywords
Subduction, collision, arcs
-> funder
Asociación Colombiana de Geólogos y Geofísicos del Petróleo, Australian Research Council
-> include model code ?
-> model code URI/DOI
No response
-> include model output data?
-> model output URI/DOI
No response
-> software framework DOI/URI
10.5281/zenodo.5606117
-> software framework source repository
https://github.com/underworldcode/UWGeodynamics
-> name of primary software framework (e.g. Underworld, ASPECT, Badlands, OpenFOAM)
No response
-> software framework authors
No response
-> software & algorithm keywords
Python, C, finite element,
-> computer URI/DOI
No response
-> add landing page image and caption
Here is a caption for the image written on a new line beneath the image link.
-> add an animation (if relevant)
No response
-> add a graphic abstract figure (if relevant)
Here is a caption for the image written on a separate line above the image link.
-> add a model setup figure (if relevant)
Here is a caption for the image written on a the same line above the image link.
-> add a description of your model setup
Here is a description of the model setup. Here is a description of the model setup. Here is a description of the model setup