Breakup Without Borders: How Continents Speed Up and Slow Down During Rifting

Abstract Relative plate motions during continental rifting result from the interplay of local with far‐field forces. Here we study the dynamics of rifting and breakup using large‐scale numerical simulations of mantle convection with self‐consistent evolution of plate boundaries. We show that contine...

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Main Authors: Martina M. Ulvrova, Sascha Brune, Simon Williams
Format: Article
Language:English
Published: Wiley 2019-02-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2018GL080387
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author Martina M. Ulvrova
Sascha Brune
Simon Williams
author_facet Martina M. Ulvrova
Sascha Brune
Simon Williams
author_sort Martina M. Ulvrova
collection DOAJ
description Abstract Relative plate motions during continental rifting result from the interplay of local with far‐field forces. Here we study the dynamics of rifting and breakup using large‐scale numerical simulations of mantle convection with self‐consistent evolution of plate boundaries. We show that continental separation follows a characteristic evolution with four distinctive phases: (1) an initial slow rifting phase with low divergence velocities and maximum tensional stresses, (2) a synrift speed‐up phase featuring an abrupt increase of extension rate with a simultaneous drop of tensional stress, (3) the breakup phase with inception of fast sea‐floor spreading, and (4) a deceleration phase occurring in most but not all models where extensional velocities decrease. We find that the speed‐up during rifting is compensated by subduction acceleration or subduction initiation even in distant localities. Our study illustrates new links between local rift dynamics, plate motions, and subduction kinematics during times of continental separation.
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spelling doaj-art-eab37756e14e41fab6700a6d5018c9ae2025-08-20T01:51:45ZengWileyGeophysical Research Letters0094-82761944-80072019-02-014631338134710.1029/2018GL080387Breakup Without Borders: How Continents Speed Up and Slow Down During RiftingMartina M. Ulvrova0Sascha Brune1Simon Williams2Institute of Geophysics ETH Zürich Zürich SwitzerlandGFZ German Research Centre for Geosciences Potsdam GermanyEarthByte Group, School of Geosciences University of Sydney Sydney New South Wales AustraliaAbstract Relative plate motions during continental rifting result from the interplay of local with far‐field forces. Here we study the dynamics of rifting and breakup using large‐scale numerical simulations of mantle convection with self‐consistent evolution of plate boundaries. We show that continental separation follows a characteristic evolution with four distinctive phases: (1) an initial slow rifting phase with low divergence velocities and maximum tensional stresses, (2) a synrift speed‐up phase featuring an abrupt increase of extension rate with a simultaneous drop of tensional stress, (3) the breakup phase with inception of fast sea‐floor spreading, and (4) a deceleration phase occurring in most but not all models where extensional velocities decrease. We find that the speed‐up during rifting is compensated by subduction acceleration or subduction initiation even in distant localities. Our study illustrates new links between local rift dynamics, plate motions, and subduction kinematics during times of continental separation.https://doi.org/10.1029/2018GL080387riftingconvectionnumerical modelingplate motionplate tectonicssupercontinent breakup
spellingShingle Martina M. Ulvrova
Sascha Brune
Simon Williams
Breakup Without Borders: How Continents Speed Up and Slow Down During Rifting
Geophysical Research Letters
rifting
convection
numerical modeling
plate motion
plate tectonics
supercontinent breakup
title Breakup Without Borders: How Continents Speed Up and Slow Down During Rifting
title_full Breakup Without Borders: How Continents Speed Up and Slow Down During Rifting
title_fullStr Breakup Without Borders: How Continents Speed Up and Slow Down During Rifting
title_full_unstemmed Breakup Without Borders: How Continents Speed Up and Slow Down During Rifting
title_short Breakup Without Borders: How Continents Speed Up and Slow Down During Rifting
title_sort breakup without borders how continents speed up and slow down during rifting
topic rifting
convection
numerical modeling
plate motion
plate tectonics
supercontinent breakup
url https://doi.org/10.1029/2018GL080387
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