АЛУНИТЫ ИЧЕТУЙСКОГО ПРОЯВЛЕНИЯ (ЗАПАДНОЕ ЗАБАЙКАЛЬЕ)
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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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