Abstract
A chronology is given for the alluvial fan deposits in the Tabernas Basin (Internal Zone, Betic Cordillera). Palaeontological and sedimentological data are used to establish a palaeoclimatic model for the Quaternary in southeastern Spain. -Authors
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CITATION STYLE
APA
Delago Castilla, L., Pascual Molina, A., & Ruiz Bustos, A. (1993). Geology and micromammals of the Serra-1 site (Tabernas Basin, Betic Cordillera). Estudios Geologicos, 49(5–6), 361–366. https://doi.org/10.3989/egeol.93495-6363
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