Estructuras pseudoanticlinales inducidas por fluidificación en la Unidad Intermedia de la cuenca de Calatayud

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dc.contributor.authorSanz Rubio, E.
dc.contributor.authorHoyos, M.
dc.contributor.authorCañaveras, J.C.
dc.contributor.authorSánchez Moral, S.
dc.date.accessioned2017-03-21T13:18:54Z
dc.date.available2017-03-21T13:18:54Z
dc.date.issued1995
dc.description.abstractSoft sediment deformation structures are described in a dolomitic palustrine-lacustrine sequence in the neogene Calatayud basin. Pseudoanticlines with associated dish structures are possibly result of a fluidization process related with groundwater saline flows proceeding from an adjacent evaporitic paleoreliefen_US
dc.identifier.urihttp://hdl.handle.net/10272/13488
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.otherDeformation structuresen_US
dc.subject.otherPseudoanticlinesen_US
dc.subject.otherFluidizationen_US
dc.subject.otherCalatayud basinen_US
dc.subject.otherMioceneen_US
dc.titleEstructuras pseudoanticlinales inducidas por fluidificación en la Unidad Intermedia de la cuenca de Calatayuden_US
dc.titlePseudoanticlines structures induced by fluidization in the Intermediate Unit of the Calatayud basineng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 18, (1995)