Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/43168
DC FieldValueLanguage
dc.contributor.authorDíaz-Hernández, José Luisen_US
dc.contributor.authorYepes, Jorgeen_US
dc.contributor.authorRomero-Díaz, Asunciónen_US
dc.contributor.authorMartín-Ramos, José Danielen_US
dc.date.accessioned2018-11-21T13:07:14Z-
dc.date.available2018-11-21T13:07:14Z-
dc.date.issued2015en_US
dc.identifier.issn0341-8162en_US
dc.identifier.urihttp://hdl.handle.net/10553/43168-
dc.description.abstractSlips are little known mud-coated structures several centimeters thick, produced by gravity-driven flows on free vertical surfaces. We have differentiated a sequence formed by three main morphologies: mud drips, slips and pseudo-stalactites. This study, located in the badlands of the Guadix and Baza basins (SE Spain), suggests that formation of muddy morphologies on subvertical walls is determined by the physico-chemical characteristics of colloidal suspensions (slurries) related to rainy periods and does not indicate any substrate decay. Multiple braided microchannels, internally structured like irregular book pages, are commonly found, each formed by mudflows during rainy episodes. These morphologies constitute a temporary sink of fine erosive materials. They consist of scarcely sorted mixtures of heterogeneous matter of a detrital-cohesive nature, with low clay contents, which inherit the features of the parent materials. The current semiarid environmental conditions appear to favor conservation rather than development. The differences observed in the slips of the Guadix and Baza basins can be determined by the different geomorphological evolution of the two basins and, to a lesser extent, by the properties of the slurries that fed the slips.en_US
dc.languageengen_US
dc.publisher0341-8162-
dc.relation.ispartofCatenaen_US
dc.sourceCatena[ISSN 0341-8162],v. 135, p. 11-21en_US
dc.subject251107 Ingeniería de suelosen_US
dc.subject250618 Sedimentologíaen_US
dc.subject250607 Geomorfologíaen_US
dc.subject.otherBadlandsen_US
dc.subject.otherGuadix–Baza basinsen_US
dc.subject.otherMud flowsen_US
dc.subject.otherNatural colloidal suspensionsen_US
dc.subject.otherSoil erosionen_US
dc.subject.otherSlippingen_US
dc.titleFeatures and evolution of slip structures in badlands areas (SE Spain)en_US
dc.typeinfo:eu-repo/semantics/Articlees
dc.typeArticlees
dc.identifier.doi10.1016/j.catena.2015.06.014
dc.identifier.scopus84938591377-
dc.identifier.isi000366225900002
dc.contributor.authorscopusid36947525700-
dc.contributor.authorscopusid16314521900-
dc.contributor.authorscopusid6506670453-
dc.contributor.authorscopusid6701394636-
dc.description.lastpage21-
dc.description.firstpage11-
dc.relation.volume135-
dc.investigacionIngeniería y Arquitecturaen_US
dc.type2Artículoen_US
dc.contributor.daisngid2254916
dc.contributor.daisngid2313783
dc.contributor.daisngid4624839
dc.contributor.daisngid2674446
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Diaz-Hernandez, JL
dc.contributor.wosstandardWOS:Yepes, J
dc.contributor.wosstandardWOS:Romero-Diaz, A
dc.contributor.wosstandardWOS:Martin-Ramos, JD
dc.date.coverdateDiciembre 2015
dc.identifier.ulpgces
dc.description.sjr1,171
dc.description.jcr2,612
dc.description.sjrqQ1
dc.description.jcrqQ1
dc.description.scieSCIE
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGIR IOCAG: Geología Aplicada y Regional-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Ingeniería Civil-
crisitem.author.orcid0000-0001-5039-1482-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameYepes Temiño, Jorge-
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