Paleosuelos con calcretas, rizolitos y Microcodium en ambientes fluviales y aluviales (Oligoceno, Prebético, provincia de Murcia)

dc.contributor.authorMolina, José Miguel
dc.contributor.authorNieto, Luis M.
dc.date.accessioned2014-03-17T13:19:24Z
dc.date.available2014-03-17T13:19:24Z
dc.date.issued2010
dc.description.abstractThe Oligocene of the Prebetic in the Jumilla-Yecla area is mainly represented by fluvial and alluvial sediments. The elementary sequence observed in these materials is made up by conglomerates, sandstones and marlstones. Intercalated in this sequence continental carbonates appear. These carbonates are characterized by the presence of rhizoliths, laminar calcretes, glaebular or nodular textures and Microcodium. These carbonates are interpreted as calcretes and their features show the great importance of the vegetation in the pedogenic origin. Then, they could be the consequence of a warm to hot climates and low, seasonal rainfall conditionsen_US
dc.identifier.urihttp://hdl.handle.net/10272/7904
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.accessRightsopen access
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherPalaeosolen_US
dc.subject.otherCalcreteen_US
dc.subject.otherMicrocodiumen_US
dc.subject.otherOligoceneen_US
dc.subject.otherPrebeticen_US
dc.titlePaleosuelos con calcretas, rizolitos y Microcodium en ambientes fluviales y aluviales (Oligoceno, Prebético, provincia de Murcia)en_US
dc.titlePalaeosols with calcretes, rhizoliths and Microcodium in fluvial and alluvial environments (Oligocene, Prebetic, Murcia province)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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