Zobrazeno 1 - 10
of 29
pro vyhledávání: '"N. V. Tsukanov"'
Autor:
A. A. Krylov, L. I. Lobkovsky, D. D. Rukavishnikova, B. V. Baranov, S. A. Kovachev, K. A. Dozorova, N. V. Tsukanov, I. P. Semiletov
Publikováno v:
Doklady Earth Sciences. 507:936-940
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b091fc396ac11aa546c72f3f0894a223
https://doi.org/10.1134/s1028334x22600591
https://doi.org/10.1134/s1028334x22600591
Publikováno v:
Oceanology. 62:528-539
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c299951f3abcd7b65df5060ff2e7a0a7
https://doi.org/10.1134/s0001437022040026
https://doi.org/10.1134/s0001437022040026
Autor:
A. A. Krylov, A. I. Ivashchenko, D. A. Ilinskiy, N. V. Tsukanov, I. P. Medvedev, Sergey A. Kovachev, N. E. Shakhova, M. E. Kulikov
Publikováno v:
Journal of Volcanology and Seismology. 14:379-393
This paper is a review of current concepts concerning the seismotectonics and seismicity in the Laptev Sea region. The chief feature of the region is a rift system extending in the shelf from the continental slope with the adjacent Gakkel Ridge to th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::984932a1210fcd00a2f4e1e734b9e16b
https://doi.org/10.1134/s0742046320060044
https://doi.org/10.1134/s0742046320060044
Publikováno v:
Доклады Академии наук. 486:354-358
The paper presents data obtained during the 69th and 72nd expeditions of the research vessel Akademik Mstislav Keldysh (2017, 2018). A mechanism of methane discharge that explains the localization of the seep fields in a limited area of the outer she
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d2303a0777556e1b94da3bf06f0616b
https://doi.org/10.31857/s0869-56524863354-358
https://doi.org/10.31857/s0869-56524863354-358
Autor:
N. V. Tsukanov, S. D. Sokolov
Publikováno v:
Russian Journal of Pacific Geology. 13:99-106
The age of the rocks of the Cretaceous volcanogenic sequence of the Alazey Plateau, Kolyma–Indigirka Orogen of Northeastern Russia, is determined using U–Pb zircon dating on trachydacites and K–Ar feldspar–groundmass dating on dacites and bas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e04e2a076cf17a210176f6a10b4a3cd
https://doi.org/10.1134/s181971401902009x
https://doi.org/10.1134/s181971401902009x
Publikováno v:
Doklady Earth Sciences. 479:290-294
The geochemistry and composition of peridotite rock-forming minerals from blocks in the serpentinite melange of Karaginskii Island have been studied. The composition features of the rock-forming minerals are indicative of the fact that they represent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f36930f91d45c514e5256dfc9b9e676d
https://doi.org/10.1134/s1028334x18030091
https://doi.org/10.1134/s1028334x18030091
Autor:
S. G. Skolotnev, N. V. Tsukanov
Publikováno v:
Doklady Earth Sciences. 478:175-178
This work presents new data on the composition of volcanics, developed within the Alazeya Plateau of the Kolyma–Indigirka fold area (Northeast Russia), which indicate essential differences in their composition and, accordingly, different geodynamic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78d05e60fd691fffa982681f081d99ff
https://doi.org/10.1134/s1028334x18020174
https://doi.org/10.1134/s1028334x18020174
Publikováno v:
Oceanology. 58:92-106
This study presents new geochemical and isotope data on igneous rocks of the Vetlovaya marginal sea paleobasin (part of the Late Mesozoic–Cenozoic margin of the northwestern Pacific). The results show that the rock complexes of this marginal sea ba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::12de1da08a2163eccf9946f5b2cf49cd
https://doi.org/10.1134/s0001437018010162
https://doi.org/10.1134/s0001437018010162
Publikováno v:
Russian Journal of Pacific Geology. 11:81-94
New data on the chemical and rare-element composition and age of the rocks referred earlier to the Iruney suite of the Kamchatka Isthmus are received. In the recent structure these rocks compose the structural–strata complexes of the nappe-folded L
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a226e2a40d6ec56c588f9355186f1b9c
https://doi.org/10.1134/s1819714017020075
https://doi.org/10.1134/s1819714017020075
Publikováno v:
Russian Journal of Pacific Geology. 8:233-246
The eastern peninsulas of Kamchatka are mostly composed of tectonostratigraphic complexes, which were formed within the Late Cretaceous-Eocene Kronotskii-Kamchatka arc. The accretion of this paleoarc to the Kamchatka margin of northeastern Asia in th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5cc4f9b4bdfe15fe2d884f3e622b81d3
https://doi.org/10.1134/s1819714014040083
https://doi.org/10.1134/s1819714014040083