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Características sedimentarias del Jurásico subbético en la región Algarinejo-Rute

Dabrio, Cristino J. and Vera, J.A. (1970) Características sedimentarias del Jurásico subbético en la región Algarinejo-Rute. Acta geologica hispanica , V (1). pp. 8-11. ISSN 0567-7505

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Abstract

Las series jurásicas de esta región muestran fuertes diferencias de facies y potencias como consecuencia de una subsidencia diferencial que se pone de manifiesto en el geosinelinal subbético a partir del Domerense.
Las series meridionales corresponden al Subbético s. str.,
mientras que las septentrionales son series de tránsito entre éste y el Subbético frontal o externo.
[ABSTRACT]
The jurassic series croping out in the surveyed region
show very conspicuous facies changes as well as thickness
variations. All these differences should be related to a differential
subsidence developed within the subbetic geosyncline
since the Domerian epoch. The southern series are belonging to the sir. s. Subbetic:
the northern ones exhibit transition features between the latter and the erterued or "frontal" Subbetic.


Item Type:Article
Subjects:Sciences > Geology > Stratigraphic geology
ID Code:10232
Deposited On:02 Mar 2010 08:09
Last Modified:02 Mar 2010 08:09

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