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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.

In: American Mineralogist, Vol. 100, No. 7, 2015.

Research output: Contribution to journal › Article

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, vol. 100, no. 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 et al. 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. In: American Mineralogist. 2015 ; Vol. 100, No. 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