Zobrazeno 1 - 10
of 53
pro vyhledávání: '"G.V. ARTEMENKO"'
Publikováno v:
Український антарктичний журнал, Iss 15, Pp 9-15 (2017)
В результате петролого-минералогических и микрозондовых исследований установлено, что сульфидная минерализация в андезитах и дацитах
Externí odkaz:
https://doaj.org/article/df1059427dc347429d86b8abe3a6cb02
Publikováno v:
Український антарктичний журнал, Iss 14, Pp 36-42 (2016)
Расслоенность интрамагматической дайки основного состава на о. Берселот обусловлена внедрением уже частично солидифицированной магмы
Externí odkaz:
https://doaj.org/article/872c8512f40a437fb007571e30392f6d
Autor:
G.V. Artemenko, L.V. Shumlyanskyy
Publikováno v:
Geological Journal. :31-44
The studied area comprises the junction zone of the Huliaipole granite-greenstone block with the Vovcha and Remivka granulitegneiss blocks. The Vovcha and Remivka blocks are composed of Archean quartz-feldspathic gneisses (>80%), also containing remn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37db747013325b873b1243c4530e33a9
https://doi.org/10.30836/igs.1025-6814.2022.4.263128
https://doi.org/10.30836/igs.1025-6814.2022.4.263128
Publikováno v:
Mineralogical Journal. 44:48-59
The Paleoproterozoic crust formation in the Azov domain remains underexplored. In the Neoarchean-Paleoproterozoic, the Azov segment of the Archean crust was fragmented by large rift structures. This stage is associated with the formation of Neoarchea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::699de640ced04b3455c09c922216104b
https://doi.org/10.15407/mineraljournal.44.02.048
https://doi.org/10.15407/mineraljournal.44.02.048
Publikováno v:
Mineralogical Journal. 44:73-83
The Middle-Dnieper megablock, which is a fragment of the craton, differs from other cratons found on Earth. This is because of the large variety of granitoids (Tokiv, Mokro-Moskowka, and Demuryne complexes) in the former that were formed after the Me
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ed93d9e738225ea21315726797faa84
https://doi.org/10.15407/mineraljournal.44.04.073
https://doi.org/10.15407/mineraljournal.44.04.073
Autor:
L.V. Shumlyanskyy, G.V. Artemenko
Publikováno v:
Reports of the National Academy of Sciences of Ukraine. :61-74
A large anticline structure occurs in the western part of the Azov Domain of the Ukrainian Shield. It is composed of rocks of the Mesoarchean (3.2-3.0 Ga) granite-greenstone association and relics of an older basement. The anticline is divided into t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b33807eba1f4141a57bff971a835aaf7
https://doi.org/10.15407/dopovidi2021.05.061
https://doi.org/10.15407/dopovidi2021.05.061
Publikováno v:
Geological Journal. :3-16
The Azov Domain occurs as a part of a larger Mesoarchean (3.2-3.0 Ga) craton, fragments of which are preserved in the eastern part of the Ukrainian Shield and as a block of the Kursk Magnetic Anomaly (KMA). In the Neoarchean-Palaeoproterozoic time, i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4efb61535a2a4a6d84b4e8f3c6410d28
https://doi.org/10.30836/igs.1025-6814.2021.1.216989
https://doi.org/10.30836/igs.1025-6814.2021.1.216989
Publikováno v:
Mineralogical Journal. 43:85-90
Results of U-Pb dating of zircons from the Middle Devonian sandstones of the Mykolaivka Suite, taken from the junction zone between the Azov Domain of the Ukrainian Shield and Donets basin, are reported. The rocks are taken from a drill core and they
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::740568a9c0d5e5d14a941d9488dd03c7
https://doi.org/10.15407/mineraljournal.43.03.085
https://doi.org/10.15407/mineraljournal.43.03.085
Autor:
G.V. ARTEMENKO, L.M. STEPANYUK, I.A. SAMBORSKA, B.V. BORODYNYA, I.A. SHVAIKA, K.I. GOGOLEV, L.I. PROSKURKA
Publikováno v:
Mineralogical Journal. 43:63-72
In the Saltych anticlinorium of the West Azov, small intrusions of rocks of basic and ultrabasic composition are known in the middle reaches of the Obitochna, Kiltychiya and Burtychiya rivers and in the upper reaches of the Obitochna river. They are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e85c6038eba2ffd4d6be4cb756ffda7b
https://doi.org/10.15407/mineraljournal.43.04.063
https://doi.org/10.15407/mineraljournal.43.04.063
Publikováno v:
Geological Journal. 372:36-46
The West Azov iron district corresponds to the Korsak synclinorium or block in which iron deposits of the Kamyana Mohyla belt (Pavlivka, Novoukrainka, and Serhiivka areas), Kuksungur, and Korsak Mohyla are located. The iron– bearing units are confi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9f283c325b8e3a89dece97ef05b7357a
https://doi.org/10.30836/igs.1025-6814.2020.3.204487
https://doi.org/10.30836/igs.1025-6814.2020.3.204487