SHORT-RANGE ORDER OF CATIONS IN NATURAL DOUBLE-CHAIN SILICATES. MARKOV-CHAIN MODELS

dc.contributor.author	Lapides I.L.
dc.contributor.author	Lustenberg E.Y.
dc.date.accessioned	2020-04-10T02:23:12Z
dc.date.available	2020-04-10T02:23:12Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30957393
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 303, 6, 119-121
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16582
dc.description.abstract	We investigated double chain silicates (amphiboles), whose structures contain three octahedral positions. A shift in the frequency of the IR vibrations of the hydroxyl group at one vertex of these octahedra was used to determine the cation population of the polyhedra, which carries information on short-range order in the unit cells of the structure. For statistical description of the sequence of cations in amphiboles we used the technique of stationary and nonstationary Markov chains of various order. The resulting statistically modeled chains represent a rather wide array of 'texts' that differ in their symbol sequences.
dc.title	SHORT-RANGE ORDER OF CATIONS IN NATURAL DOUBLE-CHAIN SILICATES. MARKOV-CHAIN MODELS
dc.type	Статья

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