The Miocene subsidence pattern of the NW Zagros foreland basin reflects the southeastward propagating tear of the Neotethys slab

<p>Tectonic processes resulting from solid Earth dynamics control uplift and generate sediment accommodation space via subsidence. Unraveling the mechanism of basin subsidence elucidates the link between deep-Earth and surface processes. The NW Zagros fold–thrust belt resulted from the Cenozoi...

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Bibliographic Details
Main Authors: R. I. Koshnaw, J. Kley, F. Schlunegger
Format: Article
Language:English
Published: Copernicus Publications 2024-11-01
Series:Solid Earth
Online Access:https://se.copernicus.org/articles/15/1365/2024/se-15-1365-2024.pdf
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