Zobrazeno 1 - 10
of 42
pro vyhledávání: '"B. A. Pokrovskii"'
Publikováno v:
Doklady Earth Sciences. 510:262-268
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7650d47845b0c907496108c79f4b72fd
https://doi.org/10.1134/s1028334x23600093
https://doi.org/10.1134/s1028334x23600093
Publikováno v:
Izvestiya, Physics of the Solid Earth. 56:675-686
Various geodynamo models proposed recently in the different ways explain the processes of geomagnetic field generation and its evolution over the course of the geological history. The testing capabilities of these models are strongly limited, inter a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::db5fea1ba8865c5bd4e91402cb7134f4
https://doi.org/10.1134/s1069351320050080
https://doi.org/10.1134/s1069351320050080
Publikováno v:
Quaternary International. 420:272-279
Two sediment cores from the Knipovich Ridge in the Fram Strait have been studied to examine paleoceanographic and climatic changes in the Polar North Atlantic during the late Middle and Late Pleistocene. As inferred from the data on foraminifers, nan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2524f6288c6c3501d1df3bc80f31f6db
https://doi.org/10.1016/j.quaint.2015.09.086
https://doi.org/10.1016/j.quaint.2015.09.086
Publikováno v:
Doklady Earth Sciences. 464:1001-1004
A stratum of glacial diamictites with thickness of up to 160 m at the basement of the sedimentary cover, overlain by a series of cap carbonates up to 40 m thick is described for several boreholes in the central regions of the Siberian platform. The i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1894d15c10d10bf793089f9e5600d76d
https://doi.org/10.1134/s1028334x15100049
https://doi.org/10.1134/s1028334x15100049
Publikováno v:
Doklady Earth Sciences. 460:11-15
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::547ba2f759db33d312ac3d4ee414beba
https://doi.org/10.1134/s1028334x15010109
https://doi.org/10.1134/s1028334x15010109
Publikováno v:
Doklady Earth Sciences. 459:1413-1417
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d1b13b3dae8768f459b25393cea56e4c
https://doi.org/10.1134/s1028334x14100079
https://doi.org/10.1134/s1028334x14100079
Publikováno v:
Lithology and Mineral Resources. 49:491-504
Variations in the carbon isotope composition in gases and waters of mud volcanoes in the Taman Peninsula are studied. The δ13C values in CH4 and CO2 vary from −59.5 to −44.0‰ (δ13Cav = −52.4 ± 5.4‰) and from −17.8 to +22.8‰ (δ13Cav
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::536ecb84bbb8ff6cc7da303f5ab413eb
https://doi.org/10.1134/s0024490214060066
https://doi.org/10.1134/s0024490214060066
Publikováno v:
Lithology and Mineral Resources. 49:519-545
Siderite microconcretions in the glauconite-bearing clayey-silty rock member of the lower sub-formation of the Khaipakh Formation (Middle Riphean, Olenek Uplift) are scrutinized for the first time. In two Khorbusuonka River sections located with a sp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28e2c2d5dd98928e7cad019d4b763c50
https://doi.org/10.1134/s0024490214060054
https://doi.org/10.1134/s0024490214060054
Publikováno v:
Lithology and Mineral Resources. 48:457-488
The Cretaceous sections of the eastern Caucasus contain rich in organic matter (OM) sediments corresponding to the late Cenomanian Oceanic Anoxic Event 2. They are marked by positive δ13C and negative δ18O isotopic anomalies, which are characterist
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7b993764bd141027f249cf094b8c4508
https://doi.org/10.1134/s0024490213060047
https://doi.org/10.1134/s0024490213060047
Autor:
B. G. Pokrovskii, V. Yu. Lavrushin, S. V. Deliya, Yu. P. Bezrodnykh, E. A. Yunin, V. V. Poshibaev
Publikováno v:
Lithology and Mineral Resources. 48:373-383
Seismoacoustic profiling and sonar survey of the North Caspian water area revealed in some areas signs of intense release of methane from the sedimentary sequence. This fact was also supported by submarine videorecording data. Such sites are characte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4fdc205cbfb06e2d860a7b245dbd2bdc
https://doi.org/10.1134/s0024490213050027
https://doi.org/10.1134/s0024490213050027