Standard

Yusupovite, Na<inf>2</inf>Zr(Si<inf>6</inf>O<inf>15</inf>)(H<inf>2</inf>O)<inf>3</inf>, a new mineral species from the Darai-Pioz alkaline massif and its implications as a new microporous filter for large ions. / Agakhanov, A.A.; Pautov, L.A.; Karpenko, V.Y.; Sokolova, E.; Abdu, Y.I.A.; Hawthorne, F.C.; Pekov, I.V.; Siidra, O.I.

в: American Mineralogist, № 7, 2015, стр. 1502-1508.

Результаты исследований: Научные публикации в периодических изданияхстатья

Harvard

APA

Vancouver

Author

Agakhanov, A.A. ; Pautov, L.A. ; Karpenko, V.Y. ; Sokolova, E. ; Abdu, Y.I.A. ; Hawthorne, F.C. ; Pekov, I.V. ; Siidra, O.I. / Yusupovite, Na<inf>2</inf>Zr(Si<inf>6</inf>O<inf>15</inf>)(H<inf>2</inf>O)<inf>3</inf>, a new mineral species from the Darai-Pioz alkaline massif and its implications as a new microporous filter for large ions. в: American Mineralogist. 2015 ; № 7. стр. 1502-1508.

BibTeX

@article{bf77f9e8125d4c03b672226de235b067,
title = "Yusupovite, Na2Zr(Si6O15)(H2O)3, a new mineral species from the Darai-Pioz alkaline massif and its implications as a new microporous filter for large ions",
abstract = "{\textcopyright} 2015 by Walter de Gruyter Berlin/Boston.Yusupovite, ideally Na2Zr(Si6O15)(H2O)3, is a new silicate mineral from the Darai-Pioz alkaline massif in the upper reaches of the Darai-Pioz river, area of the joint Turkestansky, Zeravshansky, and Alaisky ridges, Tajikistan. Yusupovite was found in a pegmatite composed mainly of reedmergnerite, aegirine, microcline, and polylithionite. It occurs as prismatic grains about 2 mm in size embedded in reedmergnerite; associated minerals are quartz, pectolite, zeravshanite, mendeleevite-(Ce), fluorite, leucosphenite, a pyrochlore-group mineral, neptunite, telyushenkoite, moskvinite-(Y), and shibkovite. Yusupovite is colorless, transparent with a white streak, has a vitreous luster, and does not fluoresce under ultraviolet light. Cleavage is perfect on {110}, parting was not observed. Mohs hardness is 5. Yusupovite is brittle with a splintery fracture. The measured and calculated densities are 2.69(2) and 2.713 g/cm",
author = "A.A. Agakhanov and L.A. Pautov and V.Y. Karpenko and E. Sokolova and Y.I.A. Abdu and F.C. Hawthorne and I.V. Pekov and O.I. Siidra",
year = "2015",
doi = "10.2138/am-2015-5092",
language = "English",
pages = "1502--1508",
journal = "American Mineralogist",
issn = "0003-004X",
publisher = "Mineralogical Society of America",
number = "7",

}

RIS

TY - JOUR

T1 - Yusupovite, Na2Zr(Si6O15)(H2O)3, a new mineral species from the Darai-Pioz alkaline massif and its implications as a new microporous filter for large ions

AU - Agakhanov, A.A.

AU - Pautov, L.A.

AU - Karpenko, V.Y.

AU - Sokolova, E.

AU - Abdu, Y.I.A.

AU - Hawthorne, F.C.

AU - Pekov, I.V.

AU - Siidra, O.I.

PY - 2015

Y1 - 2015

N2 - © 2015 by Walter de Gruyter Berlin/Boston.Yusupovite, ideally Na2Zr(Si6O15)(H2O)3, is a new silicate mineral from the Darai-Pioz alkaline massif in the upper reaches of the Darai-Pioz river, area of the joint Turkestansky, Zeravshansky, and Alaisky ridges, Tajikistan. Yusupovite was found in a pegmatite composed mainly of reedmergnerite, aegirine, microcline, and polylithionite. It occurs as prismatic grains about 2 mm in size embedded in reedmergnerite; associated minerals are quartz, pectolite, zeravshanite, mendeleevite-(Ce), fluorite, leucosphenite, a pyrochlore-group mineral, neptunite, telyushenkoite, moskvinite-(Y), and shibkovite. Yusupovite is colorless, transparent with a white streak, has a vitreous luster, and does not fluoresce under ultraviolet light. Cleavage is perfect on {110}, parting was not observed. Mohs hardness is 5. Yusupovite is brittle with a splintery fracture. The measured and calculated densities are 2.69(2) and 2.713 g/cm

AB - © 2015 by Walter de Gruyter Berlin/Boston.Yusupovite, ideally Na2Zr(Si6O15)(H2O)3, is a new silicate mineral from the Darai-Pioz alkaline massif in the upper reaches of the Darai-Pioz river, area of the joint Turkestansky, Zeravshansky, and Alaisky ridges, Tajikistan. Yusupovite was found in a pegmatite composed mainly of reedmergnerite, aegirine, microcline, and polylithionite. It occurs as prismatic grains about 2 mm in size embedded in reedmergnerite; associated minerals are quartz, pectolite, zeravshanite, mendeleevite-(Ce), fluorite, leucosphenite, a pyrochlore-group mineral, neptunite, telyushenkoite, moskvinite-(Y), and shibkovite. Yusupovite is colorless, transparent with a white streak, has a vitreous luster, and does not fluoresce under ultraviolet light. Cleavage is perfect on {110}, parting was not observed. Mohs hardness is 5. Yusupovite is brittle with a splintery fracture. The measured and calculated densities are 2.69(2) and 2.713 g/cm

U2 - 10.2138/am-2015-5092

DO - 10.2138/am-2015-5092

M3 - Article

SP - 1502

EP - 1508

JO - American Mineralogist

JF - American Mineralogist

SN - 0003-004X

IS - 7

ER -

ID: 3990746