Caracterización sedimentológica de los sistemas fluviolacustres y tobáceos del Mioceno Superior-Plioceno de la Cuenca de Calatayud (Zaragoza).

• Localización: Geogaceta, ISSN 0213-683X, Nº. 20, 2, 1996, págs. 277-281
• Idioma: español
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• Resumen

  • A complex fluviolacustrine calcareous system with associated autochtonous tufa deposits is recognized in the Upper Miocene-Pliocene of the Neogene Calatayud Basin. A detailed sedimentological analysis of the calcareous sediments reveals a wide spectrum óf facies associations mainly related to reworking of tufa deposits including products such as oncolithic tufas and less common phytoclastic and intraclastic tufas