Zobrazeno 1 - 9
of 9
pro vyhledávání: '"G. L. Leichenkov"'
Publikováno v:
Записки Горного института, Vol 224, Pp 199-199 (2017)
The paper proves the timeliness of obtaining and examining bottom sediments from subglacial Lake Vostok. Predictive geological section of Lake Vostok and information value of bottom sediments have been examined. Severe requirements towards environmen
Externí odkaz:
https://doaj.org/article/05d25f7101534d72b6750ccd141de77a
Autor:
V. V. Shcherbakova, V. Yu. Vodovozov, G. V. Zhidkov, N. A. Aphinogenova, N. V. Sal’naya, G. L. Leichenkov
Publikováno v:
Izvestiya, Physics of the Solid Earth. 58:859-881
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4463659ba659fb8bb176c4c9aaed80c7
https://doi.org/10.1134/s106935132206012x
https://doi.org/10.1134/s106935132206012x
Publikováno v:
Geochemistry International. 58:91-99
This paper reports the results of numerical estimation of the degree of organic matter maturity and hydrocarbon generation in the rocks of the Bremer 1–6 formations during the burial of the sedimentary basin of the Mawson Sea on the passive margin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e62c3d5d164d4378b2cb9c0053518f4
https://doi.org/10.1134/s001670292001005x
https://doi.org/10.1134/s001670292001005x
Publikováno v:
Физика Земли. :76-91
The paper addresses crustal formation in the Australian–Antarctic basin at the early period of separation of Australia and Antarctica. The study covers long rifting (~160–80 Ma), ultraslow spreading (~80–45 Ma) with the formation of proto-ocean
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7d73c7a153e24d91243654d413ebd00c
https://doi.org/10.31857/s0002-33372019276-91
https://doi.org/10.31857/s0002-33372019276-91
Publikováno v:
Geochemistry International. 56:554-565
This paper analyzes differences in the history of hydrocarbon (HC) generation by the rocks of the Bremer 1–6 formations in adjacent areas of the nonvolcanic passive continental margins of Australia and Antarctica. The problem is examined by the exa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::503b3e342bb9e434fb5757a26555ba39
https://doi.org/10.1134/s0016702918060046
https://doi.org/10.1134/s0016702918060046
Autor:
G. L. Leichenkov, Mikhail A Levitan
Publikováno v:
Lithology and Mineral Resources. 49:117-137
Literature pertaining to history of the Cenozoic glaciation in Antarctica and its influence on sedimentation in marginal areas of the continent and deep-water domains of the Southern Ocean are reviewed. Original data obtained by G.L. Leichenkov on se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::362c7fed013d8f579f6d914655c4c46c
https://doi.org/10.1134/s0024490214020060
https://doi.org/10.1134/s0024490214020060
Publikováno v:
Doklady Earth Sciences. 440:1207-1211
Study of mineral inclusions in the basal part of the central Antarctic ice sheet from the borehole at the Vostok station was carried out. Mineral inclusions were trapped during freezing of the subglacial Lake Vostok water on the base of the glacier,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc1d13ef89b33b1f6b0e757618c895b1
https://doi.org/10.1134/s1028334x11090054
https://doi.org/10.1134/s1028334x11090054
Publikováno v:
Geochemistry International. 47:1-17
New results on the petrochemistry and geochemistry of dolerites from the Schirmacher Oasis shed light on the development of the Karoo-Maud plume in Antarctica. The basalts and dolerites are petrologically identical to the rocks of western Dronning Ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::700c00b1bb6df1c77473a802c111a9f3
https://doi.org/10.1134/s0016702909010017
https://doi.org/10.1134/s0016702909010017
Publikováno v:
Doklady Earth Sciences. 406:128-131
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3c40d6787f508cd398332598c8f648b8
https://doi.org/10.1134/s1028334x06010314
https://doi.org/10.1134/s1028334x06010314