Oscilaciones eustáticas de alta frecuencia en el Neógeno superior de Sorbas (Almería, sureste de España)

dc.contributor.authorDabrio, Cristino José
dc.contributor.authorPolo, María Dolores
dc.date.accessioned2017-04-04T11:27:11Z
dc.date.available2017-04-04T11:27:11Z
dc.date.issued1995
dc.description.abstractA brief description of detail stratigraphy of the Late-Neogene Terminal Carbonate Complex and the Sorbas Member, and the precise role of the stromatolite layers that occur interbedded. The vicinity to the sources of coarse-gained sediment input, mobility of the sea-bottom, and the topographic elevation reached by the sea during high stands of4th/5th order oscillations control the development of stromatolites. Recognition of high-frequency (fourth and fifth-order cycles) inside a third-order (TB 3.4)'eustatic cycleen_US
dc.identifier.urihttp://hdl.handle.net/10272/13548
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherMixed shelfen_US
dc.subject.otherFringing reefsen_US
dc.subject.otherStromatolitesen_US
dc.subject.otherTalus slopeen_US
dc.subject.otherEustatic oscillationsen_US
dc.subject.otherLate Neogeneen_US
dc.subject.otherSouth-eastern Spainen_US
dc.titleOscilaciones eustáticas de alta frecuencia en el Neógeno superior de Sorbas (Almería, sureste de España)en_US
dc.titleHigh-frequency eustatic changes in the upper Neogene of Sorbas (Almería, south-eastern Spain)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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