Результаты исследований: Научные публикации в периодических изданиях › статья
Khvorovite, Pb2+4Ca2[Si8B2(SiB)O28]F, a new hyalotekite-group mineral from the Darai-Pioz alkaline massif, Tajikistan: Description and crystal structure. / Pautov, L.A.; Agakhanov, A.A.; Sokolova, E.; Hawthorne, F.C.; Karpenko, V.Y.; Siidra, O.I.; Garanin, V.K.; Abdu, Y.A.
в: Mineralogical Magazine, № 4, 2015, стр. 949-963.Результаты исследований: Научные публикации в периодических изданиях › статья
}
TY - JOUR
T1 - Khvorovite, Pb2+4Ca2[Si8B2(SiB)O28]F, a new hyalotekite-group mineral from the Darai-Pioz alkaline massif, Tajikistan: Description and crystal structure
AU - Pautov, L.A.
AU - Agakhanov, A.A.
AU - Sokolova, E.
AU - Hawthorne, F.C.
AU - Karpenko, V.Y.
AU - Siidra, O.I.
AU - Garanin, V.K.
AU - Abdu, Y.A.
PY - 2015
Y1 - 2015
N2 - © 2015 Mineralogical Society.Khvorovite, ideally Pb2+4Ca2[Si8B2(SiB)O28]F, is a new borosilicate mineral of the hyalotekite group from the Darai-Pioz alkaline massif in the upper reaches of the Darai-Pioz river, Tajikistan. Khvorovite was found in a pectolite aggregate in silexites (quartz-rich rocks). The pectolite aggregate consists mainly of pectolite, quartz and fluorite, with minor aegirine, polylithionite, turkestanite and baratovite; accessory minerals are calcite, pyrochlore-group minerals, reedmergnerite, stillwellite-(Ce), pekovite, zeravshanite, senkevichite, sokolovaite, mendeleevite-(Ce), alamosite, orlovite, leucosphenite and several unknown Cs-silicates. Khvorovite occurs as irregular grains, rarely with square or rectangular sections up to 150 μm, and grain aggregates up to 0.5 mm. Khvorovite is colourless, rarely white, transparent with a white streak, has a vitreous lustre and does not fluoresce under ultraviolet light. Cleavage and parting were not observed. Mohs hardness is 5-5.5, and khvo
AB - © 2015 Mineralogical Society.Khvorovite, ideally Pb2+4Ca2[Si8B2(SiB)O28]F, is a new borosilicate mineral of the hyalotekite group from the Darai-Pioz alkaline massif in the upper reaches of the Darai-Pioz river, Tajikistan. Khvorovite was found in a pectolite aggregate in silexites (quartz-rich rocks). The pectolite aggregate consists mainly of pectolite, quartz and fluorite, with minor aegirine, polylithionite, turkestanite and baratovite; accessory minerals are calcite, pyrochlore-group minerals, reedmergnerite, stillwellite-(Ce), pekovite, zeravshanite, senkevichite, sokolovaite, mendeleevite-(Ce), alamosite, orlovite, leucosphenite and several unknown Cs-silicates. Khvorovite occurs as irregular grains, rarely with square or rectangular sections up to 150 μm, and grain aggregates up to 0.5 mm. Khvorovite is colourless, rarely white, transparent with a white streak, has a vitreous lustre and does not fluoresce under ultraviolet light. Cleavage and parting were not observed. Mohs hardness is 5-5.5, and khvo
U2 - 10.1180/minmag.2015.079.4.06
DO - 10.1180/minmag.2015.079.4.06
M3 - Article
SP - 949
EP - 963
JO - Mineralogical Magazine
JF - Mineralogical Magazine
SN - 0026-461X
IS - 4
ER -
ID: 4013303