АЛУНИТЫ ИЧЕТУЙСКОГО ПРОЯВЛЕНИЯ (ЗАПАДНОЕ ЗАБАЙКАЛЬЕ)

dc.contributor.author	Избродин И.А.
dc.contributor.author	Рипп Г.С.
dc.contributor.author	Карманов Н.С.
dc.date.accessioned	2022-12-03T09:10:07Z
dc.date.available	2022-12-03T09:10:07Z
dc.date.issued	2005
dc.identifier	https://www.elibrary.ru/item.asp?id=9142821
dc.identifier.citation	Записки Российского минералогического общества, 2005, 134, 4, 87-97
dc.identifier.issn	0869-6055
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/40715
dc.description.abstract	Several generations of alunites with different chemical compositions were detected in Ichetuyskoye occur-rence of high aluminum rocks. Alunites are associated with pyrophyllite, muscovite, florencite, woodhouseite, svanbergite, barite, hydromica and some other minerals. There are often present Na-alunites with the higher Sr and Ca contents accompanied, simultaneously, by appearance of phosphate-ion. Composition of alunites, the ca-ses of gradual transitions between alunite and florencite, between natroalunite and its varieties enriched in Sr and Ca make evidence for widespread isomorphism of elements among cations and anions. As a result, the boundari-es between many mineral species and between groups of alunite, plumbogumite, bedantite become vague.
dc.title	АЛУНИТЫ ИЧЕТУЙСКОГО ПРОЯВЛЕНИЯ (ЗАПАДНОЕ ЗАБАЙКАЛЬЕ)
dc.type	Статья
dc.subject.udc	549.75(571.54)

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