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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| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2024-11-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/15/1365/2024/se-15-1365-2024.pdf |
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