2009
DOI: 10.2138/am.2009.3065
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Ivanyukite-Na-T, ivanyukite-Na-C, ivanyukite-K, and ivanyukite-Cu: New microporous titanosilicates from the Khibiny massif (Kola Peninsula, Russia) and crystal structure of ivanyukite-Na-T

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Cited by 38 publications
(19 citation statements)
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“…In nature, these minerals occur in natrolitised microcline–aegirine–sodalite veins within an orthoclase-bearing urtite of the Koashva apatite mine (Fig. 1), Khibiny alkaline massif, Kola Peninsula, Russia (Yakovenchuk et al , 2009). They are found in a hyperagpaitic low-temperature hydrothermal assemblage in association with natrolite, villiaumite, sitinakite, djerfisherite, sazykinaite-(Y), lucasite-(Ce), and amorphous bitumens.…”
Section: Introductionmentioning
confidence: 99%
“…In nature, these minerals occur in natrolitised microcline–aegirine–sodalite veins within an orthoclase-bearing urtite of the Koashva apatite mine (Fig. 1), Khibiny alkaline massif, Kola Peninsula, Russia (Yakovenchuk et al , 2009). They are found in a hyperagpaitic low-temperature hydrothermal assemblage in association with natrolite, villiaumite, sitinakite, djerfisherite, sazykinaite-(Y), lucasite-(Ce), and amorphous bitumens.…”
Section: Introductionmentioning
confidence: 99%
“…The ion-exchanger UOP-910, which is used for the removal of Cs-137 from radioactive-waste solutions (Anthony et al, 1994), is a natural counterpart of sitinakite, a microporous titanosilicate from hydrothermal veins of the Khibiny massif, Kola peninsula, Russia (Sokolova et al, 1989;Men'shikov et al, 1992). Another family of recently described microporous titanosilicates, the ivanyukite-group minerals (Yakovenchuk et al, 2009), have the pharmacosiderite-type structure, well known as a useful synthetic material since the 1990s (Harrison et al, 1995). There are many other unique natural titanosilicates with interesting structures that have no precedents among synthetic materials.…”
Section: Introductionmentioning
confidence: 99%
“…In addition to titanite and titanomagnetite, the apatite-nepheline deposits contain numerous pegmatites with rare titanium minerals that have important functional properties, for example, ferroelectric loparite-(Ce) [2], molecular sieve chivruaiite [3,4] (Ca-analog of synthetic microporous titanosilicate ETS-4 [5,6]), cation exchangers kukisvumite and punkaruaivite [7][8][9][10] (respectively, Zn and Li analogues of synthetic titanosilicate AM-4 [11,12]), cation exchangers sitinakite [13] (natural analogue of synthetic titanosilicate Ionsiv IE-911 [14][15][16]), and minerals of the ivanyukite group [17][18][19][20]. Besides, these and other synthetic titanium-based compounds (ETS-2, ETS-10, JDF-L1, LHT-9, MIL-125, etc.)…”
Section: Introductionmentioning
confidence: 99%
“…Moreover, ( 137 Cs, 90 Sr, 154 Eu)-exchanged forms of ivanyukite can be transformed by heating into stable SYNROC-like titanate ceramics for long-time immobilization of these radionuclides [20]. Crystal structure of ivanyukite-Na-T [17]: cubano-like clusters Ti4O24 consisting of four edgeshared TiO6 octahedra (dark-blue) are connected by vertexes SiO4 tetrahedra (yellow) to form the microporous framework, with Na (cyan), K (pale green), and H2O (magenta) in channels.…”
Section: Introductionmentioning
confidence: 99%
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