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Preliminary report on recent deposits of the Lagunas de Villafafila (Zamora)

dc.contributor.authorSantisteban, Juan Ignacio
dc.contributor.authorGarcía del Cura, María Angeles
dc.contributor.authorMediavilla López, Rosa
dc.contributor.authorDabrio, Cristino José
dc.date.accessioned2014-11-05T11:01:45Z
dc.date.available2014-11-05T11:01:45Z
dc.date.issued2002
dc.identifier.urihttp://hdl.handle.net/10272/9108
dc.description.abstractRecent sedimentation in the Lagunas de Villafafila is dominated by fine-grained sllicidastic deposits mainly composed of quartz, feldspar, muscovite, illite and kaolinite. Sediments are clay, clayey silts and clayey fine sands with sparse pedogenic carbonates and organic matter. The recentmost sediments contain diatoms and carbonates with bacterial features. Their structure is composed by parallel lamination, sometimes inclined by adaptation to bottom topography, and erosive surfaces. Rootlets are common to the top. Layering, textures and sedimentary structures reflect energy changes in the hydrological regime mainly related to water incomes from nearby areas. Although saline eflorescences are known to be generated since several millennia ago, saline layers and minerals are rare in the coresen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherSaline lakesen_US
dc.subject.otherSedimentary recorden_US
dc.subject.otherHoloceneen_US
dc.titleEstudio preliminar de los sedimentos recientes de las lagunas de Villafáfila (Zamora)en_US
dc.titlePreliminary report on recent deposits of the Lagunas de Villafafila (Zamora)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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