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Collisional Processes and Links to Episodic Changes in Subduction Zones

van Hunen, J.; Miller, M.S.

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Authors

M.S. Miller



Abstract

Continental collision is commonly accompanied by a sequence of several plate–mantle interactions, including accretion of buoyant features, pulses of slab rollback, slab break-off, formation of slab windows, and lithosphere delamination. Using the combined insight from seismic and dynamical modelling studies, we illustrate how these processes and their characteristic rates and timescales played an important role in shaping the Mediterranean and how they dominated the closure of the Tethyan oceans. Older collisions, such as the one that formed the Norwegian Caledonites, probably experienced similarly complex plate–mantle interaction, even though direct evidence of the associated mantle dynamics is absent.

Citation

van Hunen, J., & Miller, M. (2015). Collisional Processes and Links to Episodic Changes in Subduction Zones. Elements, 11(2), 119-124. https://doi.org/10.2113/gselements.11.2.119

Journal Article Type Article
Acceptance Date Nov 20, 2014
Online Publication Date Mar 31, 2015
Publication Date Apr 1, 2015
Deposit Date Nov 20, 2015
Publicly Available Date Jan 16, 2017
Journal Elements
Print ISSN 1811-5209
Electronic ISSN 1811-5217
Publisher Mineralogical Society of America
Peer Reviewed Peer Reviewed
Volume 11
Issue 2
Pages 119-124
DOI https://doi.org/10.2113/gselements.11.2.119

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