Open hvidy opened 11 months ago
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Creator/Contributor Creator/contributor is Timothy White (https://orcid.org/0000-0002-6980-3392)
Model Repository Slug
Command 'python3 .github/scripts/generate_identifier.py' returned non-zero exit status 120.
Associated Publication Found publication: The Role of Lithospheric‐Deep Mantle Interactions on the Style and Stress Evolution of Arc‐Continent Collision.
Title Title taken from associated publication The Role of Lithospheric‐Deep Mantle Interactions on the Style and Stress Evolution of Arc‐Continent Collision
Description Description taken from associated publication abstract No response
Model authors Author list taken from associated publication
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Creator/Contributor Creator/contributor is Timothy White (https://orcid.org/0000-0002-6980-3392)
Model Repository Slug
Model repo will be created with name white_2017_pleiades
Associated Publication Found publication: The Role of Lithospheric‐Deep Mantle Interactions on the Style and Stress Evolution of Arc‐Continent Collision.
Title Title taken from associated publication The Role of Lithospheric‐Deep Mantle Interactions on the Style and Stress Evolution of Arc‐Continent Collision
Description Description taken from associated publication abstract 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 Author list taken from associated publication
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Funder Funder list taken from associated publication
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-> creator/contributor ORCID (or name)
0000-0002-6980-3392
-> slug
white_2017_pleiades
-> field of Research (FoR) Codes
3706: Geophysics
-> license
CC-BY-4.0
-> model category
No response
-> associated publication DOI
https://doi.org/10.1029/2022GC010386
-> title
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-> description
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-> model authors
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-> scientific keywords
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-> funder
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-> include model code ?
-> model code URI/DOI
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-> include model output data?
-> model output URI/DOI
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-> software framework DOI/URI
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-> software framework source repository
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-> name of primary software framework (e.g. Underworld, ASPECT, Badlands, OpenFOAM)
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-> software framework authors
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-> software & algorithm keywords
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-> computer URI/DOI
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-> add landing page image and caption
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-> add an animation (if relaven)
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-> add a graphic abstract figure (if relavent)
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-> add a model setup figure (if relavent)
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-> add a description of your model setup
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