Deformation of intrasalt competent layers in different modes of salt tectonics
<p>Layered evaporite sequences (LESs) comprise interbedded weak layers (halite and, commonly, bittern salts) and strong layers (anhydrite and usually non-evaporite rocks such as carbonates and siliciclastics). This results in a strong rheological stratification, with a range of effective visco...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2019-06-01
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| Series: | Solid Earth |
| Online Access: | https://www.solid-earth.net/10/987/2019/se-10-987-2019.pdf |