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Hackman Valley, Yukspor Mt., Khibiny Massif, Kola Peninsula, Murmanskaja Oblast', Northern Region, Russia
© 2008, J. Weissman
A very large group of porous titano- and niobosilicates (monoclinic, pseudo-orthorhombic). Seven subgroups are distinguished, each corresponding to different structure types (Chukanov et al., 2002). One of these is the Nenadkevichite Subgroup which comprises orthorhombic members. |
Classification of Labuntsovite Group | |
| Dana 8th edition ID: | 60.1.3.2 60 : CYCLOSILICATES Four-Membered Rings 1 : Four-Membered Rings, as Titanosilicates |
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| mindat.org URL: | http://www.mindat.org/min-30454.html Please feel free to link to this page. |
Other Information | |
| Health Warning: | No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care. |
References for Labuntsovite Group | |
| Reference List: | Chukanov, Nikita V.; Pekov, Igor V.; Rastsvetaeva, Ramiza K.; Nekrasov, Aleksei N. (1999): Labuntsovite: solid solutions and features of the crystal structure. Can. Mineral. 37, 901-910. Chukanov, Nikita V.; Pekov, Igor V.; Khomyakov, Alexander P. (2002): Recommended nomenclature for labuntsovite-group minerals. European Journal of Mineralogy 14, 165-173. Armbruster, Th., Krivovichev, S.V., Weber, Th., Gnos, E., Organova, N.N., Yakovenchuk, V.N., Shlyukova, Z.V. (2004): Origin of diffuse superstructure reflections in labuntsovite-group minerals. American Mineralogist, 89, 1655-1666. |
Internet Links for Labuntsovite Group | |
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