hvidy / PIPE-4002-EarthByte-ModelAtlas

SIH repo for work on PIPE-4002
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[request] <feature> #13

Open hvidy opened 11 months ago

hvidy commented 11 months ago

-> 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

fig1 Landing page image caption

-> add an animation (if relevant)

animation_25 Caption for animation

-> add a graphic abstract figure (if relevant)

FranzMarc_BlueHorse Franz Marc's Blaues Pferd I

-> add a model setup figure (if relevant)

No response

-> add a description of your model setup

No response

github-actions[bot] commented 11 months ago

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

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:

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

When you have finished adding file descriptions and fixing any identified errors, please add a 'Review Requested' label to this issue.

github-actions[bot] commented 11 months ago

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

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 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.

github-actions[bot] commented 11 months ago

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

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.

github-actions[bot] commented 11 months ago

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

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.

github-actions[bot] commented 11 months ago

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.

github-actions[bot] commented 11 months ago

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

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.

github-actions[bot] commented 11 months ago

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.

hvidy commented 11 months ago

Model repository created at https://github.com/hvidy/white_2017_something_else

github-actions[bot] commented 11 months ago

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

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.

github-actions[bot] commented 11 months ago

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

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.