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
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
Andrés Felipe Rodríguez Corcho
in unexpected format. Expected last name(s), first name(s)
. 'orcid-identifier'
The following author(s) were found successfully:
Funder
The following funder(s) were found successfully:
File Manifest The files listed in the table below require descriptions. Please edit this comment to insert them into the table.
Filename | File Description |
---|---|
fig1.png | |
animation_25.gif | |
FranzMarc_BlueHorse.jpg |
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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
Field of Research (FoR) Codes 3706: Geophysics 370603: Geodesy 370605: Geothermics and radiometrics
License CC-BY-4.0
Model category
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
Andrés Felipe Rodríguez Corcho
in unexpected format. Expected last name(s), first name(s)
. 'orcid-identifier'
The following author(s) were found successfully:
Scientific keywords
Funder
'id'
The following funder(s) were found successfully:
Landing page image Filename: fig1.png Caption: Landing page image captionAnimation Filename: animation_25.gif Caption: Caption for animationGraphic abstract Filename: FranzMarc_BlueHorse.jpg Caption: Franz Marc's Blaues Pferd IModel setup figure No image uploaded. Model setup description No response When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.
Thank you for submitting. Please check the output below, and fix any errors, etc.
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
Field of Research (FoR) Codes 3706: Geophysics 370603: Geodesy 370605: Geothermics and radiometrics
License CC-BY-4.0
Model category
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
Andrés Felipe Rodríguez Corcho
in unexpected format. Expected last name(s), first name(s)
. 'orcid-identifier'
The following author(s) were found successfully:
Scientific keywords
Funder
The following funder(s) were found successfully:
Landing page image Filename: fig1.png Caption: Landing page image caption
Animation Filename: animation_25.gif Caption: Caption for animation
Graphic abstract Filename: FranzMarc_BlueHorse.jpg Caption: Franz Marc's Blaues Pferd I
Model setup figure No image uploaded.
Model setup description No response
When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.
Thank you for submitting. Please check the output below, and fix any errors, etc.
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
Field of Research (FoR) Codes 3706: Geophysics 370603: Geodesy 370605: Geothermics and radiometrics
License CC-BY-4.0
Model category
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
Andrés Felipe Rodríguez Corcho
in unexpected format. Expected last name(s), first name(s)
. 'orcid-identifier'
The following author(s) were found successfully:
Scientific keywords
Funder
The following funder(s) were found successfully:
Software Framework DOI/URI Found software: Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud.
Software Repository https://github.com/underworldcode/underworld2
Software Name Name taken from DOI record Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud
Software Framework Authors Author list taken from software DOI record
The following author(s) were found successfully:
Software & algorithm keywords No keywords given Computer URI/DOINo URI/DOI given Landing page image Filename: fig1.png Caption: Landing page image caption
Animation Filename: animation_25.gif Caption: Caption for animation
Graphic abstract Filename: FranzMarc_BlueHorse.jpg Caption: Franz Marc's Blaues Pferd I
Model setup figure No image uploaded.
Model setup description No response
When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.
Thank you for submitting. Please check the output below, and fix any errors, etc.
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
Field of Research (FoR) Codes 3706: Geophysics 370603: Geodesy
License CC-BY-4.0
Model category
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
The following author(s) were found successfully:
Scientific keywords
Funder
The following funder(s) were found successfully:
Software Framework DOI/URI Found software: Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud.
Software Repository https://github.com/underworldcode/underworld2
Software Name Name taken from DOI record Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud
Software Framework Authors Author list taken from software DOI record
The following author(s) were found successfully:
Software & algorithm keywords No keywords given
Computer URI/DOI No URI/DOI given
Landing page image Filename: fig1.png Caption: Landing page image caption
Animation Filename: animation_25.gif Caption: Caption for animation
Graphic abstract Filename: FranzMarc_BlueHorse.jpg Caption: Franz Marc's Blaues Pferd I
Model setup figure No image uploaded.
Model setup description No response
When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.
Thank you for submitting. Please check the output below, and fix any errors, etc.
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.
Field of Research (FoR) Codes 3706: Geophysics 370603: Geodesy
License CC-BY-4.0
Model category
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
The following author(s) were found successfully:
Scientific keywords
Funder
The following funder(s) were found successfully:
Software Framework DOI/URI Found software: Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud.
Software Repository https://github.com/underworldcode/underworld2
Software Name Name taken from DOI record Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud
Software Framework Authors Author list taken from software DOI record
The following author(s) were found successfully:
Software & algorithm keywords No keywords given
Computer URI/DOI No URI/DOI given
Landing page image Filename: fig1.png Caption: Landing page image caption
Animation Filename: animation_25.gif Caption: Caption for animation
Graphic abstract Filename: FranzMarc_BlueHorse.jpg Caption: Franz Marc's Blaues Pferd I
Model setup figure No image uploaded.
Model setup description No response
When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.
Thank you for submitting. Please check the output below, and fix any errors, etc.
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_something_else
Field of Research (FoR) Codes 3706: Geophysics 370603: Geodesy
License CC-BY-4.0
Model category
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
The following author(s) were found successfully:
Scientific keywords
Funder
The following funder(s) were found successfully:
Software Framework DOI/URI Found software: Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud.
Software Repository https://github.com/underworldcode/underworld2
Software Name Name taken from DOI record Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud
Software Framework Authors Author list taken from software DOI record
The following author(s) were found successfully:
Software & algorithm keywords No keywords given
Computer URI/DOI No URI/DOI given
Landing page image Filename: fig1.png Caption: Landing page image caption
Animation Filename: animation_25.gif Caption: Caption for animation
Graphic abstract Filename: FranzMarc_BlueHorse.jpg Caption: Franz Marc's Blaues Pferd I
Model setup figure No image uploaded.
Model setup description No response
When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.
Model repository created at https://github.com/hvidy/white_2017_something_else
Thank you for submitting. Please check the output below, and fix any errors, etc.
Creator/Contributor Creator/contributor is Timothy White (https://orcid.org/0000-0002-6980-3392)
Model Repository Slug
Warning: Model repo cannot be created with proposed slug white_2017_something_else
.
Either propose a new slug or repo will be created with name white_2017_something_else_1
.
Field of Research (FoR) Codes 3706: Geophysics 370603: Geodesy
License CC-BY-4.0
Model category
Associated Publication
'issue'
Title
Description
Model authors
The following author(s) were found successfully:
Scientific keywords
Funder
The following funder(s) were found successfully:
Software Framework DOI/URI Found software: Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud.
Software Repository https://github.com/underworldcode/underworld2
Software Name Name taken from DOI record Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud
Software Framework Authors Author list taken from software DOI record
The following author(s) were found successfully:
Software & algorithm keywords No keywords given
Computer URI/DOI No URI/DOI given
Landing page image Filename: fig1.png Caption: Landing page image caption
Animation Filename: animation_25.gif Caption: Caption for animation
Graphic abstract Filename: FranzMarc_BlueHorse.jpg Caption: Franz Marc's Blaues Pferd I
Model setup figure No image uploaded.
Model setup description No response
When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.
Thank you for submitting. Please check the output below, and fix any errors, etc.
Creator/Contributor Creator/contributor is Timothy White (https://orcid.org/0000-0002-6980-3392)
Model Repository Slug
Warning: Model repo cannot be created with proposed slug white_2017_something_else
.
Either propose a new slug or repo will be created with name white_2017_something_else_1
.
Field of Research (FoR) Codes 3706: Geophysics 370603: Geodesy
License CC-BY-4.0
Model category
Associated Publication
'issue'
Title
Description
Model authors
The following author(s) were found successfully:
Scientific keywords
Funder
The following funder(s) were found successfully:
Software Framework DOI/URI Found software: Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud.
Software Repository https://github.com/underworldcode/underworld2
Software Name Name taken from DOI record Underworld2: Python Geodynamics Modelling for Desktop, HPC and Cloud
Software Framework Authors Author list taken from software DOI record
The following author(s) were found successfully:
Software & algorithm keywords No keywords given
Computer URI/DOI No URI/DOI given
Landing page image Filename: fig1.png Caption: Landing page image caption
Animation Filename: animation_25.gif Caption: Caption for animation
Graphic abstract Filename: FranzMarc_BlueHorse.jpg Caption: Franz Marc's Blaues Pferd I
Model setup figure No image uploaded.
Model setup description No response
When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.
-> creator/contributor ORCID (or name)
0000-0002-6980-3392
-> slug
white_2017_something_else
-> field of Research (FoR) Codes
3706: Geophysics, 370603: Geodesy
-> license
CC-BY-4.0
-> model category
model published in study, community benchmark
-> associated publication DOI
http://dx.doi.org/10.5194/egusphere-2023-53
-> title
No response
-> description
No response
-> model authors
No response
-> scientific keywords
arc continent collision, arc buoyancy, contrasting style of collision, lithospheric flow
-> funder
https://www.arc.gov.au/, https://ror.org/05mmh0f86
-> include model code ?
-> model code URI/DOI
No response
-> include model output data?
-> model output URI/DOI
https://doi.org/10.5281/zenodo.8371229
-> software framework DOI/URI
https://doi.org/10.5281/zenodo.7455999
-> software framework source repository
https://github.com/underworldcode/underworld2
-> name of primary software framework (e.g. Underworld, ASPECT, Badlands, OpenFOAM)
No response
-> software framework authors
No response
-> software & algorithm keywords
No response
-> computer URI/DOI
No response
-> add landing page image and caption
Landing page image caption
-> add an animation (if relevant)
Caption for animation
-> add a graphic abstract figure (if relevant)
Franz Marc's Blaues Pferd I
-> add a model setup figure (if relevant)
No response
-> add a description of your model setup
No response