Eocene Gravity Flows in the Internal Prebetic (Betic Cordillera, SE Spain): A Vestige of an Ilerdian Lost Carbonate Platform in the South Iberian Margin

Eocene Gravity Flows in the Internal Prebetic (Betic Cordillera, SE Spain): A Vestige of an Ilerdian Lost Carbonate Platform in the South Iberian Margin

In the Betic-Rif Cordilleras, recent works have evidenced the existence of well-developed Eocene (Ypresian-Bartonian) carbonate platforms rich in Larger Benthic Foraminifera (LBF). Contrarily to other sectors of the western Tethys, like the Pyrenean domain in the North Iberian Margin, where these pl...

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Bibliographic Details
Main Authors: Josep Tosquella, Manuel Martín-Martín, Crina Miclăuș, José Enrique Tent-Manclús, Francisco Serrano, José Antonio Martín-Pérez
Format: Article
Language:English
Published: MDPI AG 2025-02-01
Series:Geosciences
Subjects:
lost Ilerdian carbonate platforms
Prebetic
South Iberian Margin
Eo-Alpine tectonics
microfacies characterization
Online Access:https://www.mdpi.com/2076-3263/15/3/81
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