EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Ocean subduction dynamics in the Alps

Philippe Agard1 and Mark Handy2
Philippe Agard and Mark Handy
  • 1Sorbonne Universités, UPMC Univ Paris 06, ISTEP, UMR UPMC-CNRS 7193, Paris, France (
  • 2Freie Universität Berlin, Institut für Geol. Wissensch., Berlin, D-12249, Germany

The Alps preserve abundant oceanic blueschists and eclogites that exemplify the selective preservation of fragments of relatively short-lived, small, slow-spreading North Atlantic-type ocean basins (here the ~400-700 km wide Alpine Tethys), whose subducting slabs reach down to the Mantle Transition Zone. Whereas none of the subducted fragments were returned during the first half of the subduction history, those exhumed afterwards experienced conditions typical of mature subduction zones worldwide. Sedimentary-dominated units were underplated intermittently, mostly at ~30-40 km depth, while mafic/ultramafic-dominated units subducted to ~80 km (In the W. Alps), whose protoliths had formed close to the continent, were offscraped from the slab only a few Ma before continental subduction. Spatiotemporal contrasts in burial and preservation of the fragments reveal how along-strike segmentation of the continental margin affects ocean subduction dynamics.

How to cite: Agard, P. and Handy, M.: Ocean subduction dynamics in the Alps, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-5235,, 2021.


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