Ambiente sedimentario y ciclicidad estratigráfica de los materiales de la Formación Arenas y Arcillas del Collado (Cretácico inferior), en el sector de Alpuente (Valencia)

• Autores: Carlos de Santisteban Bové
• Localización: Geogaceta, ISSN 0213-683X, Nº. 35, 2003, págs. 15-18
• Idioma: español
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• Resumen

  • The «Arenas y arcillas del Collado» Formation (Lower Cretaceous, Southwestern Iberian Basin, Valencia) represent a wave-dominated delta. It contain fluvial and shallow- marine deposits wich are arranged in two types of high-frequency sequences. The first type (up to 2 m thick) is a transgressive - regressive parasequence formed by shoreface to fluvial deposits. The second type (up to 75 m thick) is a composite depositional sequence formed by four to six parasequences. The lower part of each depositional sequence contain a progradational thick group of shoreface / foreshore sandstone units, which sharply overlies an erosional surface modified by waves during transgression.