Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2141-2020
https://doi.org/10.5194/se-11-2141-2020
Research article
 | 
18 Nov 2020
Research article |  | 18 Nov 2020

Relationship between microstructures and resistance in mafic assemblages that deform and transform

Nicolas Mansard, Holger Stünitz, Hugues Raimbourg, Jacques Précigout, Alexis Plunder, and Lucille Nègre

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Nicolas Mansard on behalf of the Authors (25 Aug 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (21 Sep 2020) by Florian Fusseis
AR by Nicolas Mansard on behalf of the Authors (24 Sep 2020)  Author's response   Manuscript 
ED: Publish as is (04 Oct 2020) by Florian Fusseis
ED: Publish as is (04 Oct 2020) by Federico Rossetti (Executive editor)
AR by Nicolas Mansard on behalf of the Authors (06 Oct 2020)  Manuscript 
Download
Short summary
Our rock deformation experiments (solid-medium Griggs-type apparatus) on wet assemblages of mafic compositions show that the ability of minerals to react controls the portions of rocks that deform and that minor chemical and mineralogical variations can considerably modify the strength of deformed assemblages. Our study suggests that the rheology of mafic rocks, which constitute a large part of the oceanic crust, cannot be summarized as being rheologically controlled by monophase materials.