HIGH DEGREE OF CATIONIC ORDERING IN THE STRUCTURE OF A NEW MINERAL OF THE LABUNTSOVITE GROUP

dc.contributor.author	Zolotarev Jr.A.A.
dc.contributor.author	Krivovichev S.V.
dc.contributor.author	Yakovenchuk V.N.
dc.contributor.author	Pakhomovsky Ya.A.
dc.contributor.author	Organova N.I.
dc.contributor.author	Armbruster T.
dc.date.accessioned	2024-11-02T11:07:42Z
dc.date.available	2024-11-02T11:07:42Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13520554
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1062-1065
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46326
dc.description.abstract	In recent years, minerals of the labuntsovite group (hereafter, LG) have become objects of many detailed mineralogical and crystallochemical studies stimulated by numerous findings of these minerals and the diversity of their chemical compositions and physicochemical properties. The LG minerals also attract interest owing to the possibility of their application in catalytic processes, adsorption, and ion exchange.
dc.subject	labuntsovite group minerals
dc.title	HIGH DEGREE OF CATIONIC ORDERING IN THE STRUCTURE OF A NEW MINERAL OF THE LABUNTSOVITE GROUP
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06070130

Files in this item

Name: Zolo_06.pdf

Size: 157.4Kb

Format: PDF