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

This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1029/2018GL080387.

Downloads

Download Preprint

Supplementary Files
Authors

Martina Ulvrova , Sascha Brune , Simon Williams 

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 syn-rift 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 seafloor 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.

DOI

https://doi.org/10.31223/osf.io/esya9

Subjects

Earth Sciences, Geophysics and Seismology, Physical Sciences and Mathematics, Tectonics and Structure

Keywords

plate tectonics, mantle convection, rifting, supercontinent breakup

Dates

Published: 2020-05-30 01:34

Older Versions
License

CC BY Attribution 4.0 International

Add a Comment

You must log in to post a comment.


Comments

There are no comments or no comments have been made public for this article.