Structure and Mechanical Properties of the Dueñas Clay Formation (Tertiary Duero Basin, Spain): An Overconsolidated Clay of Lacustrine Origin
The Dueñas Clay Formation is considered an example of a deposit of lacustrine continental origin. It is formed mainly by overconsolidated clays and includes feldspathic arenites, and clayey and silty levels; however, in geotechnical projects it is considered a clay unit and treated as a whole. The s...
Wedi'i Gadw mewn:
| Prif Awduron: | , , , , , |
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| Fformat: | Artigo |
| Iaith: | Inglês |
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MDPI AG
2021-12-01
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| Cyfres: | Applied Sciences |
| Pynciau: | |
| Mynediad Ar-lein: | https://www.mdpi.com/2076-3417/11/24/12021 |
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