2024
DOI: 10.1002/dep2.303
|View full text |Cite
|
Sign up to set email alerts
|

Tidally influenced deposits in the Río Alías Strait connecting a marginal basin with the Mediterranean Sea (Pliocene, South‐East Spain)

Fernando Sola,
Ángel Puga‐Bernabéu,
Juan C. Braga

Abstract: The Río Alías Strait developed in the Early Pliocene as a narrow marine corridor at the connection of the microtidal Mediterranean Sea and the north‐eastern margin of the Almería‐Níjar Basin in the eastern Betic Cordillera (South‐East Spain). The orientation and topography of the strait were controlled by the transpressive Carboneras and Polopos/South Cabrera fault systems. Ten sedimentary facies occur in the up to 150 m thick mixed biogenic carbonate‐terrigenous succession distinguished on the basis of their … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...

Citation Types

0
0
0

Publication Types

Select...

Relationship

0
0

Authors

Journals

citations
Cited by 0 publications
references
References 89 publications
0
0
0
Order By: Relevance

No citations

Set email alert for when this publication receives citations?