English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Zendy Pro

Presents the zaia usage as premium feature

ZAIA

Presents AI Discovery search usage as a premium feature

AI Discovery

Presents AI Discovery explain and summary usage as a premium feature

Content Analysis

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Presents the pdf analysis as premium feature

PDF Analysis

1500 Top-up

3000 Top-up

Zendy Basic

2500 Top-up

Zendy Unlimited

Presents the access of premium content as premium feature

Premium Content

Sierra Espu&#241;a is located in the Eastern Betic Cordillera. The contact between the Malaguide Complex (Internal Betic Zone) and the External Betic Zone cropouts in this area. Sierra Espu&#241;a area is a great antiformal stack that is followed by a great synforme (Mula-Pliego Depression). In the upper part of the Malaguide Complex, two nappes, with numerous internal folding and minor thrusting, are recognized: the Morron de Totana Nappe (at the bottom) and the Perona Nappe (at the top).  This structure is the result of a complex polyphasic tectonics in which two main structural events are recognized: the Intraoligocene tectonic phase, and the Lower Miocene tectonic phase.  Sierra Espu&#241;a se sit&#250;a en el sector oriental de la Cordillera B&#233;tica. En este sector afloran principalmente terrenos pertenecientes al Complejo Mal&#225;guide (Zonas Internas B&#233;ticas) en contacto con las Zonas Externas B&#233;ticas. Esta regi&#243;n se configura como un gran antiforme de mantos al S (Sierra Espu&#241;a), seguido al N por un gran sinforme (Depresi&#243;n de Mula-Pliego). En la parte alta del complejo, se reconocen dos unidades con el rango de manto de corrimiento, con numerosos repliegues y escamaciones internas: el Manto de Morr&#243;n de Totana, en posici&#243;n inferior, y el Manto de Perona, en posici&#243;n superior.  Esta estructura es el resultado de una tect&#243;nica polif&#225;sica muy compleja en la que se reconocen dos grandes eventos estructurales: la fase tect&#243;nica Intraoligocena, y la fase tect&#243;nica del Mioceno Inferior

La estructura del área de Sierra Espuña (contacto zonas internas-externas, sector oriental de la Cordillera Bética)