Zobrazeno 1 - 10
of 19
pro vyhledávání: '"D. A. Orsoev"'
Autor:
D. A. Orsoev, A. S. Mekhonoshin
Publikováno v:
Геодинамика и тектонофизика, Vol 13, Iss 4 (2022)
Mineralogical and geochemical study of the gabbro-peridotite sills located in the near-bottom part of the Yoko-Dovyren stratified massif among the host terrigenous-carbonate rocks showed that the thickest (200–250 m) of them are differentiated from
Externí odkaz:
https://doaj.org/article/2b0c8446af8c4be099ba53177bc468a9
Autor:
D. A. Orsoev
Publikováno v:
Geology of Ore Deposits. 61:306-332
Recent investigations have made it possible to update the mineralogical, petrochemical, and geochemical characteristics of anorthosites, which are considered the main link and main PGE and Au concentrator in low-sulfide PGM mineralization localized i
Autor:
E. M. Spiridonov, D. A. Orsoev, A. A. Ariskin, E. V. Kislov, N. N. Korotaeva, G. S. Nikolaev, V. O. Yapaskurt
Publikováno v:
Доклады Академии наук. 485:741-744
The Yoko-Dovyren ultramafic-mafic layered intrusion includes the Baikal deposit of Cu-Ni sulfide ores with Pt-Pd mineralization in the bottom part, and “horizons” and pockets of low-sulfide ores with Pt-Pd mineralization at the upper levels of th
Autor:
E. M. Spiridonov, D. A. Orsoev, A. A. Ariskin, E. V. Kislov, N. N. Korotaeva, G. S. Nikolaev, V. O. Yapaskurt
Publikováno v:
Геохимия. 64:554-558
The bottom part of the Yoko-Dovyren layered mafic–ultramafic intrusion hosts the Baikalskoe deposit of Cu–Ni sulfide ores with Pt–Pd mineralization, and the stratigraphically higher portion of the intrusion includes units and pockets with low-s
Autor:
N. N. Korotaeva, G. S. Nikolaev, Alexey A. Ariskin, V. O. Yapaskurt, E. M. Spiridonov, D. A. Orsoev, E. V. Kislov
Publikováno v:
Geochemistry International. 57:600-603
The bottom part of the Yoko-Dovyren layered mafic–ultramafic intrusion hosts the Baikalskoe deposit of Cu–Ni sulfide ores with Pt–Pd mineralization, and the stratigraphically higher portion of the intrusion includes units and pockets with low-s
Autor:
E. M. Spiridonov, D. A. Orsoev, A. A. Ariskin, G. S. Nikolaev, E. V. Kislov, N. N. Korotaeva, V. O. Yapaskurt
Publikováno v:
Геохимия. 64:43-58
Hg and Cd are rare chemical elements found in magmatic PGE and Au mineralization and typical of this mineralization in the Late Riphean Yoko-Dovyren plagioperidotite–troctolite–gabbronorite intrusion hosted in the Baikalides of the Baikal area. T
Autor:
E. V. Kislov, D. A. Orsoev, G. S. Nikolaev, Vasiliy O. Yapaskurt, N. N. Korotaeva, E. M. Spiridonov, Alexey A. Ariskin
Publikováno v:
Geochemistry International. 57:42-55
Hg and Cd are rare chemical elements found in magmatic PGE and Au mineralization and typical of this mineralization in the Late Riphean Yoko-Dovyren plagioperidotite–troctolite–gabbronorite intrusion hosted in the Baikalides of the Baikal area. T
Publikováno v:
Russian Geology and Geophysics. 59:472-485
We report data on the geology, mineralogy, petrography, and chemistry of 733 Ma gabbro-peridotite sills from the Late Riphean Dovyren plutonic complex. Thick sills were differentiated into plagiolherzolite to olivine gabbronorite compositions by frac
Autor:
D. A. Orsoev, R. A. Badmatsyrenova, O. K. Smirnova, I.V. Gordienko, D. V. Gorokhovsky, V. S. Lantseva
Publikováno v:
Geology of Ore Deposits. 60:1-32
Based on complex structural, rheological, and metallogenic studies, taking into account the results of earlier subject-specific, prospecting, mapping, and exploration works, it has been established that the geological structure of the district was ca
Autor:
V. O. Yapaskurt, Alexey A. Ariskin, E. M. Spiridonov, E. V. Kislov, N. N. Korotaeva, G. S. Nikolaev, D. A. Orsoev
Publikováno v:
Doklady Earth Sciences. 485:458-460
The Yoko-Dovyren ultramafic–mafic layered intrusion includes the Baikal deposit of Cu–Ni sulfide ores with Pt–Pd mineralization in the bottom part, and “horizons” and pockets of low-sulfide ores with Pt–Pd mineralization at the upper leve