@article{10272/8967,
year = {2003},
url = {http://hdl.handle.net/10272/8967},
abstract = {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 15 m thick) is a composite depositional sequence formed by four to six parasequences. The lower part of each deoositional sequence contain a progradational thick group of shoreface / foreshore sandstone units, which sharply overlies an erosional surface modified by waves during transgression},
publisher = {Sociedad Geológica de España},
keywords = {Wave-dominated delta},
keywords = {Five order ciclicity},
keywords = {Lower Cetaceous},
keywords = {Southwestern Iberian Basin},
keywords = {Valencia},
title = {Ambiente sedimentario y ciclicidad estratigrafica de los materiales de la Formacion «Arenas y ardllas del Collado» (Cretacico inferior), en el sector de Alpuente (Valencia)},
title = {Sedimentary environment and stratigraphic ciclicity of the Lower Cretaceous «Arenas y arcillas del Collado»

Formation, in Alpuente (Valencia)},
author = {Santisteban, Carlos de},
}