Comment on "the role of H3O+ in the crystal structure of illite" by F. Nieto, M. Melini, and I. Abad
Vidal, Olivier (Université Grenoble)
Dubacq, Benoît (University of Cambridge. Department of Earth Sciences)
Lanari, Pierre (Université Grenoble)

Data:	2010
Resum:	The arguments of Nieto et al. (2010) in favor of the incorporation of HO rather than HO in interlayer positions of illite are disputable. Stoichiometric arguments suggest that the excess water in the Silver Hill illite is in the form of HO. Moreover, recent thermodynamic models assuming the incorporation of interlayer HO in illite provide reasonable estimates of temperature and water content using the AEM/TEM analyses of Nieto et al. (2010).
Drets:	Tots els drets reservats.
Llengua:	Anglès
Document:	Article ; recerca ; Versió publicada
Matèria:	Composition ; Hydronium ; Illite ; Water
Publicat a:	Clays and Clay Minerals, Vol. 58, Núm. 5 (2010) , p. 717-720, ISSN 1552-8367

DOI: 10.1346/CCMN.2010.0580510

4 p, 167.2 KB  Accés restringit a la UAB

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