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El pliegue sinsedimentario de Hinojares (sector de Pozo Alcón-Tíscar, provincia de Jaén, zona externa bética)

descriptionPublicationkeyboard_double_arrow_right Article 01 Jan 2006 Spain Spanish Publisher:Sociedad Geológica de España
Authors: Sanz de Galdeano, Carlos; Galindo Zaldívar, Jesús; López Garrido, Ángel Carlos; Alfaro García, Pedro; Ruiz Bustos, A.; Marín Lechado, Carlos;

handle: 10261/29401 , 10272/8466

El pliegue sinsedimentario de Hinojares (sector de Pozo Alcón-Tíscar, provincia de Jaén, zona externa bética)

Abstract

In the proximities of Hinojares (northern border of the Guadix-Baza basin), there is a growth syncline, formed in Plio-Quaternary sediments, showing progressive unconformities in its limbs. At its ESE prolongation, the recent glacis, Pleistocene in age, shows two flexions parallel to the fold hinge and limbs. This fold has been probably controlled by the Tiscar fault and formed within a NNE-SSW compressive setting.

Este estudio ha sido financiado por los proyectos CGL200401636/BTE, CGL2004-03333/BTE, la Acción Integrada BTE2001-5230-E y el grupo RNM 217 de la Junta de Andalucía.

4 páginas, 4 figuras.-- Trabajo presentado en la 41ª Sesión Científica, Barcelona, 2006.

Peer reviewed

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Spain
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Keywords

Active Tectonics, Growth synclines, Neotectonics, Active tectonics, Growth syncline, Guadix-Baza basin, Rodent tooth

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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
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