Articles | Volume 12, issue 7
https://doi.org/10.5194/se-12-1473-2021
https://doi.org/10.5194/se-12-1473-2021
Research article
 | 
02 Jul 2021
Research article |  | 02 Jul 2021

Complex rift patterns, a result of interacting crustal and mantle weaknesses, or multiphase rifting? Insights from analogue models

Frank Zwaan, Pauline Chenin, Duncan Erratt, Gianreto Manatschal, and Guido Schreurs

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on se-2020-214', Anonymous Referee #1, 29 Jan 2021
  • RC2: 'Comment on se-2020-214', Thomas Phillips, 01 Feb 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Frank Zwaan on behalf of the Authors (21 Apr 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (29 Apr 2021) by Zoe Mildon
ED: Publish as is (30 Apr 2021) by Susanne Buiter (Executive editor)
AR by Frank Zwaan on behalf of the Authors (03 May 2021)
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Short summary
We used laboratory experiments to simulate the early evolution of rift systems, and the influence of structural weaknesses left over from previous tectonic events that can localize new deformation. We find that the orientation and type of such weaknesses can induce complex structures with different orientations during a single phase of rifting, instead of requiring multiple rifting phases. These findings provide a strong incentive to reassess the tectonic history of various natural examples.