M@TE Model Request: DOI test

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Title

DOI test

Associated Publication DOI

https://doi.org/10.1029/2022GC010386

Author(s)

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Abstract

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Keywords

1. 2. 3. ...

Field of Research (FoR) Codes

3706: Geophysics

Funder(s)

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License

CC-BY-4.0

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Associated Publication Found publication The Role of Lithospheric‐Deep Mantle Interactions on the Style and Stress Evolution of Arc‐Continent Collision.

Author(s) Author list taken from associated publication

The following author(s) were found successfully:

• Andrés Felipe Rodríguez Corcho (http://orcid.org/0000-0002-1521-7910)
• Sara Polanco (http://orcid.org/0000-0002-1270-4377)
• Rebecca Farrington (http://orcid.org/0000-0002-2594-6965)
• Romain Beucher (http://orcid.org/0000-0003-3891-5444)
• Camilo Montes (http://orcid.org/0000-0002-3553-0787)
• Louis Moresi (http://orcid.org/0000-0003-3685-174X)

Abstract Abstract taken from associated publication

AbstractWe 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. **Funder(s)** _Funder list taken from associated publication_ The following funder(s) were found successfully: - University of Melbourne **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.