Zobrazeno 1 - 10
of 22
pro vyhledávání: '"Maria Bogina"'
Autor:
V. V. Shchiptsov, Boris Belyatsky, P. V. Frolov, Evgenii Sharkov, A. V. Chistyakov, Maria Bogina
Publikováno v:
Petrology. 29:475-501
The paper reports first comprehensive geological, petrographic, mineralogical, and geochemical data on one of the world’s oldest Tiksheozero ultramafic‒alkaline‒carbonatite complex (~1.99 Ga), which belongs to the Mid-Paleoproterozoic igneous p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bfaa610fdc7c9e68f69f6fdf67c7a241
https://doi.org/10.1134/s0869591121050076
https://doi.org/10.1134/s0869591121050076
Publikováno v:
Journal of Volcanology and Seismology. 14:327-340
The study of the evolution of large igneous provinces showed that the Archean and Early Paleoproterozoic mantle plumes were formed by high-Mg ultramafic rocks and looked like thermal plumes. However, this situation experienced a cardinal change in th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b597b54b77330c13cc2051d0f8013bbf
https://doi.org/10.1134/s0742046320050061
https://doi.org/10.1134/s0742046320050061
Autor:
O. A. Bogatikov, Maria Bogina, V. V. Shchiptsov, Boris Belyatsky, A. V. Chistyakov, P. V. Frolov, Evgenii Sharkov
Publikováno v:
Doklady Earth Sciences. 486:638-643
The Tiksheozero ultramafic–alkaline–carbonatite intrusive complex, like numerous carbonatite-bearing complexes of similar composition, is a part of a large igneous province related to the ascent of a thermochemical mantle plume. The geochemical a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ccbdac9e92c48930eca8c2221b4fb3c
https://doi.org/10.1134/s1028334x19060084
https://doi.org/10.1134/s1028334x19060084
Publikováno v:
Minerals
Volume 11
Issue 6
Minerals, Vol 11, Iss 570, p 570 (2021)
Volume 11
Issue 6
Minerals, Vol 11, Iss 570, p 570 (2021)
This article reports new geochemical, Sr-Nd-Hf-Pb and Re-Os data on the rocks of the Middle Paleoproterozoic (1.99 Ga) Tiksheozero ultramafic-alkaline-carbonatite complex confined to the northeastern margin of the Karelian Craton. We focus on the poo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::50c3605b77ece07b7510af5b57ab2f67
The territory of Syria is a classic area of intraplate Neogene-Quaternary plateau basaltic magmatism (Ponikarov et al., 1969; Sharkov, 2000; Lustrino, Sharkov, 2006; Trifonov et al., 2011, etc.). These basalts belong to the Afro-Arabian large igneous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::909ed1ebd966e52ebc2ee81853909111
https://doi.org/10.5194/egusphere-egu21-7330
https://doi.org/10.5194/egusphere-egu21-7330
Most researchers believe that large igneous provinces (LIPs) are formed by adiabatic melting of heads of ascending mantle plumes. Because the LIPs have existed throughout the geological history of the Earth (Ernst, 2014), their rocks can be used to p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4cc12a53ded4040189752abd4fe780b
https://doi.org/10.5194/egusphere-egu2020-4445
https://doi.org/10.5194/egusphere-egu2020-4445
Publikováno v:
Geology of Ore Deposits. 60:172-200
Magmatic oxide mineralization widely developed in syenite–gabbro intrusive complexes is an important Fe and Ti resource. However, its origin is hotly debatable. Some researchers believe that the oxide ores were formed through precipitation of dense
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a22fec299740880c778502c28ed76b90
https://doi.org/10.1134/s1075701518020046
https://doi.org/10.1134/s1075701518020046
Publikováno v:
Geoscience Frontiers, Vol 9, Iss 1, Pp 207-221 (2018)
Compositional peculiarities of the siliceous high-Mg series (SHMS) rocks formed at the Archean–Paleoproterozoic boundary as a function of plume activity are discussed using example of Early Paleoproterozoic mafic volcanic rocks of the Vodlozero Dom
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ecb10243f7e174719dbc5e1be2863c42
https://doi.org/10.1016/j.gsf.2017.02.009
https://doi.org/10.1016/j.gsf.2017.02.009
Autor:
V. V. Shchiptsov, Boris Belyatsky, E. N. Lepekhina, A. V. Antonov, Maria Bogina, A. V. Chistyakov, Evgenii Sharkov
Publikováno v:
Petrology. 23:259-280
The paper presents a study of zircon from the Middle Paleoproterozoic Elet’ozero high-Ti layered ultramafic-mafic-alkaline intrusive complex with carbonatites and Sm-Nd isotope system of rock-forming minerals in ferrogabbro sample from this complex
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6837a29e2ad2390b96d5af35a7231b99
https://doi.org/10.1134/s0869591115030066
https://doi.org/10.1134/s0869591115030066
Publikováno v:
International Geology Review. 57:1433-1445
A combined study of major and trace elements, Nd isotopes, and U-Pb systematics has been conducted for the early Palaeoproterozoic (Sumian) volcanic rocks and granites localized in different portions of the Karelian Craton. SHRIMP dating of zircons f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44c7061c1a150424593258ba0e1fb745
https://doi.org/10.1080/00206814.2014.931783
https://doi.org/10.1080/00206814.2014.931783