Zobrazeno 1 - 10
of 24
pro vyhledávání: '"D. Yu. Pushcharovskii"'
Publikováno v:
Geology of Ore Deposits. 63:805-811
Autor:
Ivan V. Podborodnikov, A. M. Dymshits, Anton Shatskiy, Konstantin D. Litasov, Igor S. Sharygin, E. Otani, D. Yu. Pushcharovskii
Publikováno v:
Doklady Earth Sciences. 461:273-276
The results of studies of the P-V-T equations of state (EOS) of Na-pyroxene using the multi-anvil technique and synchrotron radiation at pressures up to 15.3 GPa and temperatures up to 1673 K are presented. By fitting the Birch-Murnaghan EOS, the fol
Autor:
D. Yu. Pushcharovskii, Dmitry A. Ksenofontov, I. A. Ekimenkova, Igor V. Pekov, Yu. K. Kabalov, Natalia V. Zubkova
Publikováno v:
Doklady Earth Sciences. 456:520-523
The crystal structure of fornacite Pb2(Cu,Fe)[CrO4(As,P)O4OH] from the Berezovskii deposit (Central Urals, Russia) was refined by X-ray powder diffraction data using the Rietveld method. Fornacite is monoclinic, space group P21/c, the unit cell dimen
Autor:
D. Yu. Pushcharovskii, Günter Blass, Igor V. Pekov, Natalia V. Zubkova, H. Prinz, Nikita V. Chukanov
Publikováno v:
Doklady Earth Sciences. 449:342-345
Autor:
Vasiliy O. Yapaskurt, Igor V. Pekov, Michael Zelenski, D. Yu. Pushcharovskii, D. Yu. Chernyshov, Natalia V. Zubkova
Publikováno v:
Doklady Earth Sciences. 448:112-116
A new Cu-rich variety of lyonsite has been found from fumarolic sublimates of the Tolbachik volcano (Kamchatka, Russia). The empirical formula is Cu4.33Fe2.373+Ti0.26Al0.26Zn0.07(V5.85As0.07Mo0.07P0.01S0.01)O24. The crystal structure was studied on s
Publikováno v:
Moscow University Geology Bulletin. 66:221-224
Publikováno v:
Doklady Earth Sciences. 439:998-1001
Autor:
Nikita V. Chukanov, Josef-Christian Buhl, Dmitry A. Ksenofontov, Natalia V. Zubkova, Wulf Depmeier, Igor V. Pekov, D. Yu. Pushcharovskii
Publikováno v:
Doklady Earth Sciences. 438:669-672
Autor:
D. Yu. Pushcharovskii, E. I. Gerasimova, Nikita V. Chukanov, V. O. Yapaskurt, A. E. Zadov, Igor V. Pekov, Natalia V. Zubkova, Yu. K. Kabalov, V. M. Gekimyants
Publikováno v:
Doklady Earth Sciences. 436:230-236
Hydroxylchondrodite was found in the Perovski� tovaya Kop’ on the western slope of the Chuvashskie Mountains in the Zlatoust region of the Southern Urals (Russia). It is located in the contact zone between magnesium skarn and host marble being in
Publikováno v:
Doklady Earth Sciences. 427:814-818
Using X-ray analysis, the crystal structure of yegorovite Na4[Si4O8(OH)4] · 7H2O, a newly-discovered mineral from the Lovozero alkaline complex (Kola Peninsula, Russia), was determined. The mineral is monoclinic, of P21/c, a = 9.8744(4), b = 12.3981