hvidy / PIPE-4002-EarthByte-ModelAtlas

SIH repo for work on PIPE-4002
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[request] <feature> #12

Open hvidy opened 11 months ago

hvidy commented 11 months ago

-> 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

No response

-> description

No response

-> model authors

No response

-> 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

No response

-> 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)

No response

-> software framework authors

No response

-> 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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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

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

The following author(s) were found successfully:

Funder Funder list taken from associated publication

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

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

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

The following author(s) were found successfully:

Funder Funder list taken from associated publication

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

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