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Mineralogical characteristics ofHolocene alluvial sediments from the Barranco Grande (Bardenas Reales ofNavarra)

dc.contributor.authorBastida, Joaquín
dc.contributor.authorOsácar, María Cinta
dc.contributor.authorMuñoz Jiménez, Arsenio
dc.contributor.authorSancho, Carlos
dc.description.abstractMineralogical composition of Holocene alluvial deposits from Bardenas Reales of Navarra is studied and compared with the Miocene mudrock substratum. An Early Holocene muddy-silty unit and another Middle-Upper Holocene sandy unit can be differentiated. Mineralogy semiquantitative results are compatible with weak weathering processes affecting the parent materials under humid conditions prior to Holocene. Besides, differences between alluvial units can be explained in terms of bedrock weathering, sedimentary features, recyclingofsediments and pedogenetic processesen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.subject.otherBardenas Realesen_US
dc.titleCaracterísticas mineralógicas de los sedimentos aluviales holocenos del Barranco Grande (Bardenas Reales de Navarra)en_US
dc.titleMineralogical characteristics ofHolocene alluvial sediments from the Barranco Grande (Bardenas Reales ofNavarra)eng

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Atribución-NoComercial-SinDerivadas 3.0 España
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