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Subduction and Slab Detachment in the Mediterranean-Carpathian Region

Wortel, M. J. R., Spakman, W.·2000·Science

Abstract

Seismic tomography models of the three-dimensional upper mantle velocity structure of the Mediterranean-Carpathian region provide a better understanding of the lithospheric processes governing its geodynamical evolution. Slab detachment, in particular lateral migration of this process along the plate boundary, is a key element in the lithospheric dynamics of the region during the last 20 to 30 million years. It strongly affects arc and trench migration, and causes along-strike variations in vertical motions, stress fields, and magmatism. In a terminal-stage subduction zone, involving collision and suturing, slab detachment is the natural last stage in the gravitational settling of subducted lithosphere.

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Metadata

Authors
Wortel, M. J. R., & Spakman, W.
Venue
Science
Published
2000-12-08
Volume
290
Issue
5498
Pages
1910-1917
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2064893459
Cited by
1,626
References
0
FWCI
25.33
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Subduction and Slab Detachment in the Mediterranean-Carpathian Region. https://app.cochat.ai/papers/10.1126/science.290.5498.1910
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Wortel, M. J. R., & Spakman, W. (2000). Subduction and Slab Detachment in the Mediterranean-Carpathian Region. Science. https://doi.org/10.1126/science.290.5498.1910

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.