Resumen: 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.
