Zobrazeno 1 - 10
of 13
pro vyhledávání: '"V. I. Levitskii"'
Autor:
A. N. Sapozhnikov, N. V. Chukanov, R. Yu. Shendrik, M. F. Vigasina, V. L. Tauson, S. V. Lipko, D. I. Belakovskiy, V. I. Levitskii, L. F. Suvorova, L. A. Ivanova
Publikováno v:
Geology of Ore Deposits. 64:470-475
Autor:
Nikita V. Chukanov, Vladimir L. Tauson, L. F. Suvorova, Roman Shendrik, A. N. Sapozhnikov, S. V. Lipko, Marina F. Vigasina, V. I. Levitskii
Publikováno v:
American Mineralogist. 106:226-234
Dark blue lazurite from the Malo-Bystrinskoe lazurite deposit, Baikal Lake area, Eastern Siberian region, Russia, was analyzed by electron microprobe and revealed an unusually high content of total sulfur corresponding to 8.3 wt% S. The relative cont
Autor:
Alexander V. Ignatiev, Elena I. Demonterova, V. I. Levitskii, A. I. Khanchuk, I. V. Levitskii, T. A. Velivetskaya, S. V. Vysotskiy
Publikováno v:
Doklady Earth Sciences. 491:238-242
The present paper presents new U–Pb and Sm–Nd age data obtained for granulites of the Cheremshanskaya Unit enclosing metamorphosed volcano-sedimentary sulfide ores, in which sulfur isotope mass-independent fractionation (MIF–S) was established.
Autor:
V. I. Levitskii, A.V. Aseeva, T. A. Velivetskaya, A. V. Ignat’ev, A. S. Mekhonoshin, S. V. Vysotskiy, I.V. Levitskii
Publikováno v:
Russian Geology and Geophysics. 60:862-875
—We present results of study of sulfide ore occurrence in highly metamorphosed (granulite facies) Archean rocks of the Siberian craton basement. The host rocks and ore minerals are briefly described, and new data on the multiple sulfur isotope (δ3
Autor:
Vladislav Powerman, Ivan V. Levitskii, Ludmila Pavlova, Elena I. Demonterova, V. I. Levitskii, Fernando Corfu, Vadim S. Kamenetsky, L. Z. Reznitskii, V. M. Savatenkov, Alexei V. Ivanov
Publikováno v:
Lithos. :88-100
The Siberian Craton assembled in a Paleoproterozoic episode at about 1.88 Ga by the collision older blocks, followed at about 1.86 Ga by post-collisional felsic magma. We have found a set of extremely fresh mica-bearing lamprophyre-looking rocks with
Autor:
S. V. Vysotskiy, Tatiana A. Velivetskaya, Sergey Y. Budnitskiy, V. V. Yakovenko, Alexander V. Ignatiev, V. I. Levitskii
Publikováno v:
Chemical Geology. 493:316-326
A new laser ablation method has been developed for measurements of multiple sulfur isotopes in sulfides using a femtosecond laser ablation system in combination with a reactor for sulfide aerosol conversion into SF6 gas, a cryogenic and chromatograph
Autor:
V. I. Levitskii, E. N. Terekhov, S. V. Vysotskii, A. V. Ignat’ev, T. A. Velivetskaya, A. I. Khanchuk
Publikováno v:
Doklady Earth Sciences. 469:867-869
The first data on the multi-isotope composition of sulfur (32S, 33S, 34S) in samples from the Fennoscandian Shield were obtained by the laser local method. An anomalous concentration of the stable isotope 33S was registered in some samples. Δ33S ran
Autor:
S. V. Vysotskiy, A. V. Ignat’ev, V. I. Levitskii, V. V. Yakovenko, T. A. Velivetskaya, Victor P. Nechaev
Publikováno v:
Geochemistry International. 52:773-782
aka corundumbearing zones have extremely low δ 18 O (lower than -26‰) and δ D (lower than -215‰), which suggest that the mineralforming process involved gl acial waters and that the minerals preserve the iso� topic ratios of their protolith.
Autor:
E. O. Dubinina, I. V. Levitskii, G. V. Konstantinova, Igor M. Gorokhov, V. I. Levitskii, T. L. Turchenko, A. B. Kuznetsov
Publikováno v:
Doklady Earth Sciences. 455:341-345
341 The Onot greenstone belt (OGB) forms a trough (paleorift) structure within the Prisayan marginal block of the Siberian Platform basement (Fig. 1). The OGP occurs on ancient tonalite–trondhjemite–gran odiorite gneiss containing zircons with a
Autor:
V. I. Levitskii, V. P. Kovach, N. A. Sergeeva, N. G. Rizvanova, L. K. Levskii, O. A. Levchenkov
Publikováno v:
Petrology. 20:86-92
New geochronological (U-Pb, Pb-LS, Sm-Nd) studies were carried out for minerals from metamorphic rocks (aluminous plagiogneisses with sillimanite (kinzigites) and potassium shadow migmatites) to establish the sequence of metamorphic events in the Irk