Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Evgeny V. Sklyarov"'
Publikováno v:
Russian Geology and Geophysics. 60:1229-1246
—A continuous solid-solution series between the end-members eskolaite (98 wt.% Cr2O3) and karelianite (93 wt.% V2O3) has been revealed in Cr–V-bearing rocks of the Slyudyanka metamorphic complex. Chromium and vanadium oxides crystallized as karel
Autor:
Evgeny V. Sklyarov, Z. F. Ushchapovskaya, L. F. Suvorova, L. Z. Reznitsky, I. G. Barash, Thomas Armbruster, Georgia Cametti
Publikováno v:
Geology of Ore Deposits. 60:607-615
A new mineral was discovered in Cr–V-bearing marbles of the Sludyanka Complex from the Pereval marble quarry, Sludyanka district, southern Baikal region, Russia. It was named vanadio-pargasite as vanadium-bearing analog of pargasite according to th
Autor:
Evgeny V. Sklyarov, Thomas Armbruster, Georgia Cametti, Giancarlo Della Ventura, L. Z. Reznitsky
Publikováno v:
European Journal of Mineralogy. 30:981-987
The crystal structure of a new member of the calcium amphibole subgroup, vanadio-pargasite ideally NaCa2(Mg4V3+)Si6Al2O22(OH)2 with empirical formula (K0.07Na0.90)(Na0.05Ca1.91Mg0.04)Σ2.00(Mg4.02Cr0.05V0.68Al0.23Ti0.02)Σ5.00(Si6.09Al1.91)Σ8.00O22(
Publikováno v:
European Journal of Mineralogy. 21:885-891
The crystal structures of three different solid-solution members between the new mineral oxyvanite (V3O5) - and berde- sinskiite (V2TiO5) from a quartzite rock in the Pereval marble quarry of the Sludyanka complex, south of Lake Baikal (Russia), have
Publikováno v:
European Journal of Mineralogy. 20:975-981
The crystal structure (space group P 1, a = 7.5208(4), b = 7.6430(4), c = 9.5724(4) A, α= 110.204(3), β = 103.338(6), γ= 98.281(7)°, V = 487.14(7) A 3 , Z = 1) of the new mineral batisivite, (V, Cr) 8 Ti 6 [Ba(Si 2 O 7 )]O 22 , has been determine
Publikováno v:
Island Arc. 16:224-242
The Oka Belt, composed of clastic rocks and greenschists, extends for approximately 600 km in the South-Siberian Sayan region and adjacent northern Mongolia. For a long time the Oka Belt’s age and tectonic setting were the most controversial proble
Publikováno v:
American Mineralogist. 91:196-202
A new occurrence of schreyerite, V 2 Ti 3 O 9 , has recently been found in metamorphic rocks of the Sludyanka complex at the southern shore of Lake Baikal, Russia. In contrast to previously known schreyerite lamellae, whichare intergrown with rutile,