Please use this identifier to cite or link to this item: http://hdl.handle.net/10201/97647

Title: Morfología Fluvial.-Vertisols (as paleosols) with its related gigants land cracks as a disaster in central Iran deserts
Date of creation: Sep-2009
Related subjects: CDU::5 - Ciencias puras y naturales::55 - Geología. Meteorología
Keywords: land cracks
land depression
vertisols
paleoclimates
desert futures
Central Iran
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.
Primary author: Akhavan Ghalibaf, M.
Alhoseini Almodarresi, B.B.S
Faculty / Departments / Services: Universidad de Murcia
Published in: Congreso Internacional sobre desertificación
URI: http://hdl.handle.net/10201/97647
Document type: info:eu-repo/semantics/other
Number of pages / Extensions: 4
Rights: info:eu-repo/semantics/openAccess
Attribution-NonCommercial-NoDerivatives 4.0 International
Appears in Collections:Congreso Internacional sobre Desertificación.



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