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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. / Agakhanov, Atali A.; Pautov, Leonid A.; Karpenko, Vladimir Y.; Sokolova, Elena; Abdu, Yassir A.; Hawthorne, Frank C.; Pekov, Igor V.; Siidra, Oleg I.

в: American Mineralogist, Том 100, № 7, 2015.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Agakhanov, AA, Pautov, LA, Karpenko, VY, Sokolova, E, Abdu, YA, Hawthorne, FC, Pekov, IV & Siidra, OI 2015, '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', American Mineralogist, Том. 100, № 7.

APA

Agakhanov, A. A., Pautov, L. A., Karpenko, V. Y., Sokolova, E., Abdu, Y. A., Hawthorne, F. C., Pekov, I. V., & Siidra, O. I. (2015). 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. American Mineralogist, 100(7).

Vancouver

Agakhanov AA, Pautov LA, Karpenko VY, Sokolova E, Abdu YA, Hawthorne FC и пр. 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. American Mineralogist. 2015;100(7).

Author

Agakhanov, Atali A. ; Pautov, Leonid A. ; Karpenko, Vladimir Y. ; Sokolova, Elena ; Abdu, Yassir A. ; Hawthorne, Frank C. ; Pekov, Igor V. ; Siidra, Oleg I. / 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. в: American Mineralogist. 2015 ; Том 100, № 7.

BibTeX

@article{38e7822b5bd74855a162f57133e9ba60,
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 = "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(3), respectively. Yusupovite is optically biaxial (+) with refractive indices (lambda = 589 nm) al",
author = "Agakhanov, {Atali A.} and Pautov, {Leonid A.} and Karpenko, {Vladimir Y.} and Elena Sokolova and Abdu, {Yassir A.} and Hawthorne, {Frank C.} and Pekov, {Igor V.} and Siidra, {Oleg I.}",
year = "2015",
language = "English",
volume = "100",
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, Atali A.

AU - Pautov, Leonid A.

AU - Karpenko, Vladimir Y.

AU - Sokolova, Elena

AU - Abdu, Yassir A.

AU - Hawthorne, Frank C.

AU - Pekov, Igor V.

AU - Siidra, Oleg I.

PY - 2015

Y1 - 2015

N2 - 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(3), respectively. Yusupovite is optically biaxial (+) with refractive indices (lambda = 589 nm) al

AB - 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(3), respectively. Yusupovite is optically biaxial (+) with refractive indices (lambda = 589 nm) al

M3 - Article

VL - 100

JO - American Mineralogist

JF - American Mineralogist

SN - 0003-004X

IS - 7

ER -

ID: 4038190