Publication:
Características sedimentarias del Jurásico subbético en la región Algarinejo-Rute

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1970
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Instituto Nacional de Geología. Instituto Jaime Almera
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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.
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