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¿Por qué son tan diferentes las sierras de Crevillente y Abanilla?

Authors: Tent Manclús, José Enrique; Yébenes, Alfonso; Estévez, Antonio;

¿Por qué son tan diferentes las sierras de Crevillente y Abanilla?

Abstract

The Crevillente and Abanilla mountain ranges form the same structural lineation but show a quite different morphology. The first one is made by calcareous rocks mainly jurassic and cretaceous likewise the Abanilla is made by keuper facies which includes blocks. This keuper facies are not Triassic but Miocene which are interpreted as an ancient salt glacier. Their different litologies of both sierras is due to the activity of the Puerto de Barinas Fault, a transverse fault to the Crevillente-Abanilla lineament. This litological difference in the same structural lineament could be explained as produced before (pre-late Tortonian) the elevation of both sierras (latest Messinian).

Este trabajo ha sido realizado en el marco del proyecto BTE 2003-01113 y del grupo de investigación GRUPOS03/085 (Generalitat Valenciana).

Country
Spain
Related Organizations
Keywords

Puerto de Barinas fault, Miocene, Fortuna Basin, Eastern Betic Cordillera

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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
0
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