Paleokarstificación en facies yesíferas e implicaciones sedimentarias. Ejemplos del Mioceno de la Cuenca de Madrid

dc.contributor.authorRodríguez Aranda, J. Pablo
dc.contributor.authorCalvo, J. Pedro
dc.contributor.authorSanz Montero, María Esther
dc.date.accessioned2016-05-31T11:32:09Z
dc.date.available2016-05-31T11:32:09Z
dc.date.issued1996
dc.description.abstractPaleokarst surfaces developed in gypsum deposits are present in two distinct situations within the Miocene evaporite formations of the Madrid Basin: 1) paleokarst surfaces related to major sedimentary breaks and 2) incipient paleokarsts at the tops of the evaporite sedimentary sequences (sedimentary diastems). The karstification features are varied and include small dolines, networks of chimneys and fissures as well as collapse frameworks. Emphasis is placed on the role of bush vegetation in promoting dissolutional features of the gypsum karst, which is clearly evidenced within the sedimentary diastemsen_US
dc.identifier.urihttp://hdl.handle.net/10272/12201
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.otherPaleokarsten_US
dc.subject.otherGypsumen_US
dc.subject.otherMioceneen_US
dc.subject.otherMadrid Basinen_US
dc.titlePaleokarstificación en facies yesíferas e implicaciones sedimentarias. Ejemplos del Mioceno de la Cuenca de Madriden_US
dc.titleGypsum paleokarst and its sedimentary significance. Examples from Miocene formations of the Madrid Basineng
dc.typejournal articleen_US
dspace.entity.typePublication

Files

Original bundle

Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
Paleokarstificacion.pdf
Size:
343.42 KB
Format:
Adobe Portable Document Format