1995
DOI: 10.1346/ccmn.1995.0430213
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Definition of Clay and Clay Mineral: Joint Report of the Aipea Nomenclature and CMS Nomenclature Committees

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Cited by 303 publications
(169 citation statements)
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“…Clays as assemblies of silicate minerals are proper candidates for key elements in prebiotic evolution, since they can replicate and can form a dynamic basis for the assembly of poly-alpha-aminoacids and poly-nucleotides in the process of the polymerization to oligomers (Ferris, 1996;Guggenheim, 1995;Hashizume, 2012). Yet polymerization alone is not sufficient: also a distinct functional sequence of the particular eISSN 1303-5150 www.neuroquantology.com 115 building blocks is required.…”
Section: Electromagnetic Signaling Properties Of Clay Under Quantum Cmentioning
confidence: 99%
“…Clays as assemblies of silicate minerals are proper candidates for key elements in prebiotic evolution, since they can replicate and can form a dynamic basis for the assembly of poly-alpha-aminoacids and poly-nucleotides in the process of the polymerization to oligomers (Ferris, 1996;Guggenheim, 1995;Hashizume, 2012). Yet polymerization alone is not sufficient: also a distinct functional sequence of the particular eISSN 1303-5150 www.neuroquantology.com 115 building blocks is required.…”
Section: Electromagnetic Signaling Properties Of Clay Under Quantum Cmentioning
confidence: 99%
“…Bentonite refers to a naturally occurring material which consists primarily of fine-grained particles, which is generally plastic at appropriate water contents and hardens when it is dried or fired [1]. Major clay minerals in bentonites are smectites, such as montmorillonite, beidellite, saponite, nontronite, and hectorite [1]- [3].…”
Section: Introductionmentioning
confidence: 99%
“…Major clay minerals in bentonites are smectites, such as montmorillonite, beidellite, saponite, nontronite, and hectorite [1]- [3]. Two types of octahedral sheets occur in smectites: the dioctahedral type, where two-thirds of the octahedral sites are occupied mainly by trivalent cations, e.g., Al (III) or Fe (III), and the trioctahedral type, with most of the sites occupied by divalent cations, e.g., Mg (II).…”
Section: Introductionmentioning
confidence: 99%
“…The JNCs have proposed the term a class of hydrated phyllosilicates forming the fine-grained fraction of rocks, sediments, and soils and have defined 'clay' as ''a naturally occurring material composed primarily of fine-grained minerals, which is generally plastic at appropriate water contents and will harden when dried or fired'' [1]. According to this definition synthetic clays and clay-like materials are not regarded as clay even though they may be fine grained, and display the attributes of plasticity and hardening on drying and firing.…”
Section: Introductionmentioning
confidence: 99%