COMPOSITIONS OF THE APATITE-GROUP MINERALS: SUBSTITUTION MECHANISMS AND CONTROLLING FACTORS

dc.contributor.author	Pan Y.
dc.contributor.author	Fleet M.E.
dc.date.accessioned	2021-10-14T07:45:25Z
dc.date.available	2021-10-14T07:45:25Z
dc.date.issued	2002
dc.identifier	https://elibrary.ru/item.asp?id=14322226
dc.identifier.citation	Reviews in Mineralogy and Geochemistry, 2002, 48, , 48
dc.identifier.issn	1529-6466
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/30703
dc.description.abstract	The apatite-group minerals of the general formula, M10(ZO4)6X2 (M = Ca, Sr, Pb, Na…, Z = P, As, Si, V…, and X = F, OH, Cl…), are remarkably tolerant to structural distortion and chemical substitution, and consequently are extremely diverse in composition (e.g., Kreidler and Hummel 1970; McConnell 1973; Roy et al. 1978; Elliott 1994). Of particular interest is that a number of important geological, environmental/paleoenvironmental, and technological applications of the apatite-group minerals are directly linked to their chemical compositions. It is therefore fundamentally important to understand the substitution...
dc.title	COMPOSITIONS OF THE APATITE-GROUP MINERALS: SUBSTITUTION MECHANISMS AND CONTROLLING FACTORS
dc.type	Статья

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