dc.creatorBouza, Pablo Jose
dc.date.accessioned2020-01-27T17:21:13Z
dc.date.accessioned2022-10-15T13:12:31Z
dc.date.available2020-01-27T17:21:13Z
dc.date.available2022-10-15T13:12:31Z
dc.date.created2020-01-27T17:21:13Z
dc.date.issued2009-04
dc.identifierBouza, Pablo Jose; Reply to Vogt's comments on the paper "Fibrous-clay mineral formation and soil evolution in Aridisols of northeastern Patagonia, Argentina" by P.J. Bouza, M. Simón, J. Aguilar, H. del Valle and M. Rostagno; Elsevier Science; Geoderma; 150; 1-2; 4-2009; 228-229
dc.identifier0016-7061
dc.identifierhttp://hdl.handle.net/11336/95837
dc.identifierCONICET Digital
dc.identifierCONICET
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4390020
dc.description.abstractVogt's comments emphasize the potential influence that the cryogenic processes could have had on the genesis of the soils analyzed in this study. We really appreciate her comments. Indeed, we took into consideration and cited one of her studies dealing with cryogenic processes and sepiolite formation. However, our results led us to conclusions different to the ones held by Vogt.
dc.languageeng
dc.publisherElsevier Science
dc.relationinfo:eu-repo/semantics/altIdentifier/doi/http://dx.doi.org/10.1016/j.geoderma.2009.01.018
dc.relationinfo:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S0016706109000378
dc.rightshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.rightsinfo:eu-repo/semantics/restrictedAccess
dc.subjectSEPIOLITE
dc.subjectPALYGORSKITE
dc.subjectPEDOGENIC ORIGIN
dc.subjectCALCRETES
dc.titleReply to Vogt's comments on the paper "Fibrous-clay mineral formation and soil evolution in Aridisols of northeastern Patagonia, Argentina" by P.J. Bouza, M. Simón, J. Aguilar, H. del Valle and M. Rostagno
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:ar-repo/semantics/artículo
dc.typeinfo:eu-repo/semantics/publishedVersion


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