Zobrazeno 1 - 10
of 23
pro vyhledávání: '"G.I. Batova"'
Publikováno v:
Russian Geology and Geophysics. 62:460-473
––The main factors controlling the bulk sedimentation in the Siberian segment of the Lomonosov Ridge (axial part and western slope) and the Laptev Sea continental margin during the late Cenozoic were studied using a complex of geomorphological, l
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d40488d0199ab70030a7277551d37985
https://doi.org/10.2113/rgg20194137
https://doi.org/10.2113/rgg20194137
Publikováno v:
Russian Geology and Geophysics. 61:444-455
—The main factors controlling the bulk sedimentation in the region of the Mendeleev Rise and the adjacent part of the Arctic Ocean during the late Cenozoic were studied using a complex of geomorphological, lithological, and organic geochemical data
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::012e8e8a8f74c1c21b927366269385f1
https://doi.org/10.15372/rgg2019084
https://doi.org/10.15372/rgg2019084
Publikováno v:
Russian Geology and Geophysics. 58:322-331
Samples of Triassic sediments were collected from cores of parametric boreholes drilled on the Admiralteiskii Rise, Franz Josef Land Archipelago, and Fersman structure in the northeastern part of the Barents Sea sedimentary basin. The composition and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fdc9d84a74bcb983e22eef428229f20f
https://doi.org/10.1016/j.rgg.2016.09.008
https://doi.org/10.1016/j.rgg.2016.09.008
Autor:
A. V. Kursheva, G.I. Batova, A.V. Rusinovich, I. V. Litvinenko, V. I. Petrova, I.P. Morgunova
Publikováno v:
Neftegazovaya Geologiya. Teoriya I Praktika. 13
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d76d86522c68000c496bab5397297ca6
https://doi.org/10.17353/2070-5379/23_2018
https://doi.org/10.17353/2070-5379/23_2018
Publikováno v:
Geochemistry International. 48:140-151
The lateral variability of main geochemical parameters of dispersed organic matter (DOM) in the bottoms sediments of the Ob Bay was studied using materials of areal geological survey. It was found that they correspond to background compositions of es
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5ae3c0b0ce6f594d5e0763609d1f8a7a
https://doi.org/10.1134/s0016702910020035
https://doi.org/10.1134/s0016702910020035
Publikováno v:
Russian Geology and Geophysics. 51:88-97
Based on geomorphological, lithological, and facial characteristics of the East Arctic continental margin, we studied the main factors controlling the Late Cenozoic supply of organic matter (OM) to the bottom sediments of the Central Arctic rises of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c179edc1d68a6be0edb453bdf2839279
https://doi.org/10.1016/j.rgg.2009.12.008
https://doi.org/10.1016/j.rgg.2009.12.008
Geochemistry of polycyclic aromatic hydrocarbons in the bottom sediments of the eastern Arctic shelf
Autor:
I. V. Litvinenko, Vladimir M Savinov, V. I. Petrova, G.I. Batova, T. N. Savinova, A. V. Kursheva
Publikováno v:
Oceanology. 48:196-203
Sources and pathways of supply of polycyclic aromatic hydrocarbons (PAH) in the surface sediments of the Laptev and East Siberian seas were identified based on an analysis of the lithological-geochemical characteristics and distribution of organic ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7165cddeb0c3a7fd862177a57bcd1cd5
https://doi.org/10.1134/s0001437008020057
https://doi.org/10.1134/s0001437008020057
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
K zobrazení výsledku je třeba se přihlásit.
K zobrazení výsledku je třeba se přihlásit.