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Morfología Fluvial.-Vertisols (as paleosols) with its related gigants land cracks as a disaster in central Iran deserts

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dc.contributor.authorAkhavan Ghalibaf, M.
dc.contributor.authorAlhoseini Almodarresi, B.B.S
dc.contributor.otherUniversidad de Murciaes
dc.date.accessioned2020-10-26T12:49:13Z
dc.date.available2020-10-26T12:49:13Z
dc.date.created2009-09
dc.description.abstractABSTRACT This paper discuses the genesis of land cracks and land depression as one of the clayey desert futures in Central Iran. The origin of this future has been issued after downfall of ground water pressure. The clay mineralogy showed that the swelling clays of smectite groups (like as beidellite) as vertisols can be mainspring for this limitation future in Central Iran. It concluded that pedogenesis in the paleoclimates was effective to form these smectite groups of minerals in paleosoils of Yazd, Central Iran.es
dc.formatapplication/pdfes
dc.format.extent4es
dc.identifier.urihttp://hdl.handle.net/10201/97647
dc.languageenges
dc.relationSin financiación externa a la Universidad de Murciaes
dc.relation.ispartofCongreso Internacional sobre desertificaciónes
dc.rightsinfo:eu-repo/semantics/openAccesses
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 International*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subjectland crackses
dc.subjectland depressiones
dc.subjectvertisolses
dc.subjectpaleoclimateses
dc.subjectdesert futureses
dc.subjectCentral Iranes
dc.subject.otherCDU::5 - Ciencias puras y naturales::55 - Geología. Meteorologíaes
dc.titleMorfología Fluvial.-Vertisols (as paleosols) with its related gigants land cracks as a disaster in central Iran desertses
dc.typeinfo:eu-repo/semantics/otheres
dspace.entity.typePublicationes
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Congreso Internacional sobre Desertificación.