Structure and Mechanical Properties of the Dueñas Clay Formation (Tertiary Duero Basin, Spain): An Overconsolidated Clay of Lacustrine Origin

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...

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Bibliographic Details
Main Authors: José Nespereira, José Antonio Blanco, Mercedes Suárez, Emilia García-Romero, Mariano Yenes, Serafín Monterrubio
Format: Article
Language:English
Published: MDPI AG 2021-12-01
Series:Applied Sciences
Subjects:
overconsolidated clays
continental
structure
geotechnical properties
lacustrine
Dueñas Clay
Online Access:https://www.mdpi.com/2076-3417/11/24/12021

Internet

https://www.mdpi.com/2076-3417/11/24/12021

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