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

Akhavan Ghalibaf, M.; Alhoseini Almodarresi, B.B.S

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Campo DC	Valor	Lengua/Idioma
dc.contributor.author	Akhavan Ghalibaf, M.	-
dc.contributor.author	Alhoseini Almodarresi, B.B.S	-
dc.contributor.other	Universidad de Murcia	es
dc.date.accessioned	2020-10-26T12:49:13Z	-
dc.date.available	2020-10-26T12:49:13Z	-
dc.date.created	2009-09	-
dc.identifier.uri	http://hdl.handle.net/10201/97647	-
dc.description.abstract	ABSTRACT 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.format	application/pdf	es
dc.format.extent	4	es
dc.language	eng	es
dc.relation	Sin financiación externa a la Universidad de Murcia	es
dc.relation.ispartof	Congreso Internacional sobre desertificación	es
dc.rights	info:eu-repo/semantics/openAccess	es
dc.rights	Attribution-NonCommercial-NoDerivatives 4.0 International	*
dc.rights.uri	http://creativecommons.org/licenses/by-nc-nd/4.0/	*
dc.subject	land cracks	es
dc.subject	land depression	es
dc.subject	vertisols	es
dc.subject	paleoclimates	es
dc.subject	desert futures	es
dc.subject	Central Iran	es
dc.subject.other	CDU::5 - Ciencias puras y naturales::55 - Geología. Meteorología	es
dc.title	Morfología Fluvial.-Vertisols (as paleosols) with its related gigants land cracks as a disaster in central Iran deserts	es
dc.type	info:eu-repo/semantics/other	es
Aparece en las colecciones:	Congreso Internacional sobre Desertificación.

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