Ikorskyite KMn<sup>3+</sup>(Si<sub>4</sub>O<sub>10</sub>)·3H<sub>2</sub>O — new mineral from the Khibiny alkaline massif (Kola peninsula, Russia)

Ikorskyite KMn3+(Si4O10)·3H2O is new mineral from agpaitic pegmatite of the Kukisvumchorr Mt. (Khibiny Massif, Russia). The mineral forms radial aggregates of light-brown crystals growing on separate quartz crystals or on romanèchite crusts in association with barite, donneite-Y, strontionite, natrolite, vinogradovite, manganoneptunite and organic matter. The mineral is monoclinic, space group P21/c. a = 5.0714(3), b = 8.2731(5), c = 13.3740(11) Å, β = 93.730(5)°, V = 559.93(5) Å3. The eight most intense lines of the diffractogram are: (I-d[Å]-hkl): 55-7.04-011; 41-4.318-110; 100-4.185-11-1; 24-3.956-021; 28-3.339-004; 19-3.095-014; 30-3.014-113; 70-2.939-12-2. The crystal structure of ikorskyite belongs to a new structure type of minerals and inorganic compounds and belongs to the palygorskite group. The mineral is named in honor of Serafim Veniaminovich Ikorsky (1927–2016), a well-known specialist in the field of organic matter and gases research of the Kola alkaline province.

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Journal
Zapiski RMO (Proceedings of the Russian Mineralogical Society)
Published
2024-08-11
DOI
https://doi.org/10.31857/s0869605524010041
Primary Topic
Crystal Structures and Properties
Type
article
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article

Ikorskyite KMn3+(Si4O10)·3H2O — new mineral from the Khibiny alkaline massif (Kola peninsula, Russia)

Vladimir N. Bocharov, Julia A. Mikhailova, Yevgeny E. Savchenko, N. G. Konoplyova et al.
Zapiski RMO (Proceedings of the Russian Mineralogical Society)
Crystal Structures and Properties
article

Ikorskyite KMn3+(Si4O10)·3H2O — new mineral from the Khibiny alkaline massif (Kola peninsula, Russia)

Vladimir N. Bocharov, Julia A. Mikhailova, Yevgeny E. Savchenko, N. G. Konoplyova, Dar’ya V. Spiridonova, Taras L. Panikorovskii, S. V. Krivovichev, V. N. Yakovenchuk, Yakov A. Pakhomovsky
article en

Abstract

Ikorskyite KMn3+(Si4O10)·3H2O is new mineral from agpaitic pegmatite of the Kukisvumchorr Mt. (Khibiny Massif, Russia). The mineral forms radial aggregates of light-brown crystals growing on separate quartz crystals or on romanèchite crusts in association with barite, donneite-Y, strontionite, natrolite, vinogradovite, manganoneptunite and organic matter. The mineral is monoclinic, space group P21/c. a = 5.0714(3), b = 8.2731(5), c = 13.3740(11) Å, β = 93.730(5)°, V = 559.93(5) Å3. The eight most intense lines of the diffractogram are: (I-d[Å]-hkl): 55-7.04-011; 41-4.318-110; 100-4.185-11-1; 24-3.956-021; 28-3.339-004; 19-3.095-014; 30-3.014-113; 70-2.939-12-2. The crystal structure of ikorskyite belongs to a new structure type of minerals and inorganic compounds and belongs to the palygorskite group. The mineral is named in honor of Serafim Veniaminovich Ikorsky (1927–2016), a well-known specialist in the field of organic matter and gases research of the Kola alkaline province.

Zapiski RMO (Proceedings of the Russian Mineralogical Society)Vol. CLIII(1)
St Petersburg University (RU), Kola Science Centre (RU)
Life below water
Openalex Percentile: Top 88%
Crystal Structures and Properties
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Ikorskyite KMn<sup>3+</sup>(Si<sub>4</sub>O<sub>10</sub>)·3H<sub>2</sub>O — new mineral from the Khibiny alkaline massif (Kola peninsula, Russia) — Vladimir N. Bocharov, Julia A. Mikhailova, et al. · Zapiski RMO (Proceedings of the Russian Mineralogical Society) (2024) | TGRS Research Map | TGRS