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

Sanz de Galdeano, Carlos; Galindo Zaldívar, Jesús; López Garrido, Ángel Carlos; Alfaro García, Pedro; Ruiz Bustos, A.; Marín Lechado, Carlos

The Hinojares synsedimentary fold (Pozo Alcón-Tíscar area, Jaen province, Betic External Zone)

Author

Sanz de Galdeano, Carlos; Galindo Zaldívar, Jesús; López Garrido, Ángel Carlos; Alfaro García, Pedro; Ruiz Bustos, A.; [et al.]
Publication Date

2006
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
URI

http://hdl.handle.net/10272/8466

Fichero	Tamaño	Formato	Ver	Description
El-pliegue.pdf	199.7Kb	PDF	View/Open

Fichero	Tamaño	Formato	Ver	Description
El-pliegue.pdf	199.7Kb	PDF	View/Open

This item appears in the following Collection(s)

Geogaceta -- Nº 41, (2006)

Statistics

View Usage Statistics

Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

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

The Hinojares synsedimentary fold (Pozo Alcón-Tíscar area, Jaen province, Betic External Zone)

Author

Sanz de Galdeano, Carlos; Galindo Zaldívar, Jesús; López Garrido, Ángel Carlos; Alfaro García, Pedro; Ruiz Bustos, A.; [et al.]

Publication Date

2006

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

URI

http://hdl.handle.net/10272/8466

Fichero	Tamaño	Formato	Ver	Description
El-pliegue.pdf	199.7Kb	PDF	View/Open

Fichero	Tamaño	Formato	Ver	Description
El-pliegue.pdf	199.7Kb	PDF	View/Open

This item appears in the following Collection(s)

Geogaceta -- Nº 41, (2006)