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What are the required conditions to trigger the obduction/subduction initiation?

Authors :
Yamato, Philippe
Duretz, Thibault
Agard, Philippe
Soret, Mathieu
Géosciences Rennes (GR)
Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 1 (UR1)
Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES)
Institute of Geology and Palaeontology
Université de Lausanne (UNIL)
Institut des Sciences de la Terre de Paris (iSTeP)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)
European Geosciences Union
Dubigeon, Isabelle
Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)
Université de Rennes (UR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 2 (UR2)-Centre National de la Recherche Scientifique (CNRS)-Institut National de Recherche pour l’Agriculture, l’Alimentation et l’Environnement (INRAE)-Centre National de la Recherche Scientifique (CNRS)
Université de Lausanne = University of Lausanne (UNIL)
Source :
European Geosciences Union General Assembly 2016, European Geosciences Union General Assembly 2016, Apr 2016, Vienne, Austria. Geophysical Research Abstracts, 18, pp.EGU2016-4768, 2016
Publication Year :
2016
Publisher :
HAL CCSD, 2016.

Abstract

International audience; The initial stages allowing for the birth of obduction and/or subduction zones still remain enigmatic and highlydebated. Although there is no doubt that initiation occurs on a preexisting lithospheric-scale thermal or mechanicaldiscontinuity (e.g., ridge, supra-subduction zone or transform fault), no consensus has yet been reached onthis subject. However, more and more data allowing to address this issue are available (coming from field analyses,metamorphic petrology and geochronology). In particular, metamorphic soles located at the base of ophioliticnappes, which formed during the very first stages of initiation, yield increasingly precise P-T-t constraints. By confrontingsuch data to thermo-mechanical models, it should be possible to identify which initial configuration allowsfor metamorphic sole formation and for the emplacement (or not) of an ophiolitic nappe of realistic dimensions.In this study we designed thermo-mechanical models encompassing three initial model configurations, for whichP-T-t data from the Semail ophiolite of Oman are then used for the validation of model outputs. The first configurationencompasses an oceanic ridge type initial thermal perturbation (error function). The second configurationmimics the thermal perturbation caused by the arrival of a mantle plume at the base of the lithosphere (gaussianfunction). The third initial condition corresponds to a case where the obduction/subduction initiates along a transformfault delimitating lithospheres of contrasting thermal ages (step function).Our results show that obduction never initiates in ridge type models, excepted for particular conditions that are notcompatible with the Oman case. They also indicate that the initial thermal anomaly has to be sharp but not necessaryof large amplitude and that the strength of the lithosphere has to be high enough to ensure the establishment ofthin and long ophiolitic nappe without buckling. Our results also highlight the key role of shear heating in enablingobduction/subduction initiation.

Details

Language :
English
Database :
OpenAIRE
Journal :
European Geosciences Union General Assembly 2016, European Geosciences Union General Assembly 2016, Apr 2016, Vienne, Austria. Geophysical Research Abstracts, 18, pp.EGU2016-4768, 2016
Accession number :
edsair.dedup.wf.001..ca9dfea5df50f07ef4ae5718bfc66865