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Vigrishinite, Zn2Ti4 − xSi4O14(OH,H2O,□)8, a new mineral from the Lovozero alkaline complex, Kola Peninsula, Russia

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TLDR
Vigrishinite as mentioned in this paper is an epistolite-group member and first layer titanosilicate with species-defining Zn, which was found at Mt. Malyi Punkaruaiv, in the Lovozero alkaline complex, Kola Peninsula, Russia.
Abstract
A new mineral vigrishinite, epistolite-group member and first layer titanosilicate with species-defining Zn, was found at Mt. Malyi Punkaruaiv, in the Lovozero alkaline complex, Kola Peninsula, Russia. It occurs in a hydrothermally altered peralkaline pegmatite and is associated with microcline, ussingite, aegirine, analcime, gmelinite-Na, and chabazite-Ca. Vigrishinite forms rectangular or irregularly shaped lamellae up to 0.05 × 2 × 3 cm flattened on [001]. They are typically slightly split and show blocky character. The mineral is translucent to transparent and pale pink, yellowish-pinkish or colorless. The luster is vitreous. The Mohs’ hardness is 2.5–3. Vigrishinite is brittle. Cleavage is {001} perfect. Dmeas = 3.03(2), Dcalc = 2.97 g/cm3. The mineral is optically biaxial (−), α = 1.755(5), β = 1.82(1), γ = 1.835(8), 2Vmeas = 45(10)°, 2Vcalc = 50°. IR spectrum is given. The chemical composition (wt %; average of 9 point analyses, H2O is determined by modified Penfield method) is as follows: 0.98 Na2O, 0.30 K2O, 0.56 CaO, 0.05 SrO, 0.44 BaO, 0.36 MgO, 2.09 MnO, 14.39 ZnO, 2.00 Fe2O3, 0.36 Al2O3, 32.29 SiO2, 29.14 TiO2, 2.08 ZrO2, 7.34 Nb2O5, 0.46 F, 9.1 H2O, −0.19 O=F2, total is 101.75. The empirical formula calculated on the basis of Si + Al = 4 is: H7.42(Zn1.30Na0.23Mn0.22Ca0.07Mg0.07K0.05Ba0.02)Σ1.96(Ti2.68Nb0.41Fe0.183+Zr0.12)Σ3.39(Si3.95Al0.05)Σ420.31F0.18. The simplified formula is: Zn2Ti4−xSi4O14(OH,H2O,□)8 (x < 1). Vigrishinite is triclinic, space group P\(\bar 1\), a = 8.743(9), b = 8.698(9), c = 11.581(11)A, α = 91.54(8)°, β = 98.29(8)°, γ = 105.65(8)°, V = 837.2(1.5) A3, Z = 2. The strongest reflections in the X-ray powder pattern (d, A, −I[hkl]) are: 11.7-67[001], 8.27-50[100], 6.94-43[0\(\bar 1\)1, \(\bar 1\)10], 5.73–54[1\(\bar 1\)1, 002], 4.17-65[020, \(\bar 1\)\(\bar 1\)2, 200], and 2.861-100[3\(\bar 1\)0, 2\(\bar 2\)2, 004, 1\(\bar 3\)1]. The crystal structure model was obtained on a single crystal, R = 0.171. Vigrishinite and murmanite are close in the structure of the TiSiO motif, but strongly differ from each other in part of large cations and H-bearing groups. Vigrishinite is named in honor of Viktor G. Grishin (b. 1953), a Russian amateur mineralogist and mineral collector, to pay tribute to his contribution to the mineralogy of the Lovozero Complex. The type specimen is deposited in the Fersman Mineralogical Museum of Russian Academy of Sciences, Moscow.

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The seidozerite supergroup of TS-block minerals: nomenclature and classification, with change of the following names: rinkite to rinkite-(Ce), mosandrite to mosandrite-(Ce), hainite to hainite-(Y) and innelite-1T to innelite-1A

TL;DR: In this paper, a nomenclature and classification for the seidozerite-supergroup minerals is presented, where the TS block is characterized by a planar minimal cell based on translation vectors, t1 and t2.
Journal ArticleDOI

Calciomurmanite, (Na,□)2Ca(Ti,Mg,Nb)4[Si2O7]2O2(OH,O)2(H2O)4, a new mineral from the Lovozero and Khibiny alkaline complexes, Kola Peninsula, Russia

TL;DR: Calciomurmanite as discussed by the authors, a Na-Ca ordered analogue of murmanite, has been found in three localities at Kola Peninsula, Russia: at Mt. Flora in the Lovozero alkaline complex (the holotype) and at Mts. Eveslogchorr and Koashva, both in the Khibiny alkyaline complex.
Journal ArticleDOI

Crystal chemistry of cation-exchanged forms of epistolite-group minerals. Part II. Vigrishinite and Zn-exchanged murmanite

TL;DR: In this paper, the crystal structure of vigrishinite, an epistolite-group heterophyllosilicate with essential Zn, has been reinvestigated, the ideal end-member formula is revised to Zn 2 Ti 4− x (Si 2 O 7 ) 2 O 2 (OH,F,O) 2 (H 2 O,OH,□) 4 with x 4 solution at 90°C.
Journal ArticleDOI

From structure topology to chemical composition. XXIII. Revision of the crystal structure and chemical formula of zvyaginite, Na2ZnTiNb2(Si2O7)2O2(OH)2(H2O)4, a seidozerite-supergroup mineral from the Lovozero alkaline massif, Kola peninsula, Russia

Abstract: The crystal structure and chemical formula of zvyaginite, ideally Na2ZnTiNb2(Si2O7)2O2(OH)2(H2O)4, a lamprophyllite-group mineral of the seidozerite supergroup from the type locality, Mt. Malyi Punkaruaiv, Lovozero alkaline massif, Kola Peninsula, Russia have been revised. The crystal structurewas refined with a new origin in space group C1, a = 10.769(2), b = 14.276(3), c = 12.101(2) A, α = 105.45(3), β = 95.17(3), γ = 90.04(3)°, V = 1785.3(3.2) A3, R1 = 9.23%. The electron-microprobe analysis gave the following empirical formula [calculated on 22 (O + F)]: (Na0.75Ca0.09K0.04□1.12)Σ2 (Na1.12Zn0.88Mn0.17Fe2+ 0.04□0.79)Σ3 (Nb1.68Ti1.25Al0.07)Σ3 (Si4.03O14)O2 [(OH)1.11F0.89]Σ2(H2O)4, Z = 4. Electron-diffraction patterns have prominent streaking along c* and HRTEM images show an intergrowth of crystalline zvyaginite with two distinct phases, both of which are partially amorphous. The crystal structure of zvyaginite is an array of TS (Titanium-Silicate) blocks connected via hydrogen bonds between H2O groups. The TS block consists of HOH sheets (H = heteropolyhedral, O = octahedral) parallel to (001). In the O sheet, the [6]MO(1,4,5) sites are occupied mainly by Ti, Zn and Na and the [6]MO(2,3) sites are occupied by Na at less than 50%. In the H sheet, the [6]MH(1,2) sites are occupied mainly by Nb and the [8]AP(1) and [8]AP(2) sites are occupied mainly by Na and □. The MH and AP polyhedra and Si2O7 groups constitute the H sheet. The ideal structural formula is Na□Nb2NaZn□Ti(Si2O7)2O2(OH)2(H2O)4. Zvyaginite is a Zn-bearing and Na-poor analogue of epistolite, ideally (Na□)Nb2Na3Ti(Si2O7)2O2(OH)2(H2O)4. Epistolite and zvyaginite are related by the following substitution in the O sheet of the TS-block: (Naþ 2 )epi↔Zn2+ zvy +□zvy. The doubling of the t1 and t2 translations of zvyaginite relative to those of epistolite is due to the order of Zn and Na along a (t1) and b (t2) in the O sheet of zvyaginite.
References
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Journal ArticleDOI

A short history of SHELX

TL;DR: This paper could serve as a general literature citation when one or more of the open-source SH ELX programs (and the Bruker AXS version SHELXTL) are employed in the course of a crystal-structure determination.
Book

Mineralogy of Hyperagpaitic Alkaline Rocks

TL;DR: Hyperagpaitic rocks are a type of pegmatoid formation in nepheline syenite massifs as mentioned in this paper, and water-soluble and unstable minerals are major constituents and indicators of hyperagpatheric rocks.
BookDOI

Minerals as advanced materials I

TL;DR: In this article, a new mineral called Chivruaiite, a new type of Titanosilicates with ion-exchange properties, was described and its properties were investigated.
Journal ArticleDOI

Polysomatic Aspects of Microporous Minerals – Heterophyllosilicates, Palysepioles and Rhodesite-Related Structures

TL;DR: Ferraris et al. as discussed by the authors presented three groups of microporous minerals emphasizing the modular aspects of their crystal structures and the role that modularity plays in correlating different structures as well as structure and properties.
Journal ArticleDOI

Crystal-structure refinement of a Zn-rich kupletskite from Mont Saint-Hilaire, Quebec, with contributions to the geochemistry of zinc in peralkaline environments

TL;DR: Zn-rich kupletskite is triclinic, P1¯, a = 5.3765(4), b = 11.6997(10), a = 113.070(3), b= 94.775(2), g = 103.0570 for 3757 observed reflections with Fo > 4 s(Fo) as mentioned in this paper.
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