1997
DOI: 10.1180/claymin.1997.032.3.11
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Report of the Association Internationale pour l'Etude des Argiles (AIPEA) Nomenclature Committee for 1996

Abstract: The most recent report of the AIPEA Nomenclature Committee involved the definition and use of the terms 'clay' and 'clay mineral'; see Guggenheim & Martin (1995; 1996). Additional items acted upon by this committee are reported here.

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Cited by 12 publications
(7 citation statements)
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“…As recommended by Guggenheim et al (1997), these two terms are used hereafter as mineral names even though both species are in fact polytypes. Kaolin is used hereafter as a mineral group name to describe the subgroup of dioctahedral 1:1 phyllosilicates.…”
Section: K a O L I N I N S A N D S T O N E D I A G E N E S I Smentioning
confidence: 99%
“…As recommended by Guggenheim et al (1997), these two terms are used hereafter as mineral names even though both species are in fact polytypes. Kaolin is used hereafter as a mineral group name to describe the subgroup of dioctahedral 1:1 phyllosilicates.…”
Section: K a O L I N I N S A N D S T O N E D I A G E N E S I Smentioning
confidence: 99%
“…The vermiculite in comparison with mica has a lower layer charge and the iron is oxidized. Vermiculites are generally termed (according to the joint nomenclature committees AIPEA and CMS) on the basis of a negative layer charge, which is higher than 0.6 while for smectites it is between 0.2 and 0.6 per half unit cell (Guggenheim et al, 1997;Guggenheim et al, 2006;Bergaya and Lagaly, 2006). The negative layer charge of montmorillonites results from an octahedral substitution of magnesium by iron because of the sporadic tetrahedral substitution of Al 3+ for Si 4+ (Grim and Kulbicky, 1961).…”
Section: Introductionmentioning
confidence: 99%
“…hydroxide sheet Mg6(OH) Vermiculites are generally trioctahedral and are termed (according to the joint nomenclature committees AIPEA and CMS) on the basis of a negative layer charge, which is between 0.6 to 0.9 p.f.u. [4,7,8]. The negative layer charge of vermiculites results from the substitution of Si 4+ by trivalent cations in tetrahedral positions [9,10].…”
Section: Layer Charge (X) Per Half Unit Cellmentioning
confidence: 99%