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Extrusion of subducted crust explains the emplacement of far-travelled ophiolites

Kristóf Porkoláb (), Thibault Duretz, Philippe Yamato, Antoine Auzemery and Ernst Willingshofer
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Kristóf Porkoláb: Utrecht University
Thibault Duretz: Univ Rennes, CNRS, Géosciences Rennes
Philippe Yamato: Univ Rennes, CNRS, Géosciences Rennes
Antoine Auzemery: Utrecht University
Ernst Willingshofer: Utrecht University

Nature Communications, 2021, vol. 12, issue 1, 1-11

Abstract: Abstract Continental subduction below oceanic plates and associated emplacement of ophiolite sheets remain enigmatic chapters in global plate tectonics. Numerous ophiolite belts on Earth exhibit a far-travelled ophiolite sheet that is separated from its oceanic root by tectonic windows exposing continental crust, which experienced subduction-related high pressure-low temperature metamorphism during obduction. However, the link between continental subduction-exhumation dynamics and far-travelled ophiolite emplacement remains poorly understood. Here we combine data collected from ophiolite belts worldwide with thermo-mechanical simulations of continental subduction dynamics to show the causal link between the extrusion of subducted continental crust and the emplacement of far-travelled ophiolites. Our results reveal that buoyancy-driven extrusion of subducted crust triggers necking and breaking of the overriding oceanic upper plate. The broken-off piece of oceanic lithosphere is then transported on top of the continent along a flat thrust segment and becomes a far-travelled ophiolite sheet separated from its root by the extruded continental crust. Our results indicate that the extrusion of the subducted continental crust and the emplacement of far-travelled ophiolite sheets are inseparable processes.

Date: 2021
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DOI: 10.1038/s41467-021-21866-1

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