Zobrazeno 1 - 9
of 9
pro vyhledávání: '"A.Yu. Bekker"'
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:
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
Publikováno v:
Reports of the National Academy of Sciences of Ukraine. :54-60
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb0c763507b43634f2078d08c9608c89
https://doi.org/10.15407/dopovidi2020.06.054
https://doi.org/10.15407/dopovidi2020.06.054
Publikováno v:
Reports of the National Academy of Sciences of Ukraine. 12:65-74
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43727cc7fa9f76d05b273b6a4be943d3
https://doi.org/10.15407/dopovidi2019.12.065
https://doi.org/10.15407/dopovidi2019.12.065
The U-Pb age of zircon populations from metadacite of the Huliaipole Suite was determined using the LA-ICP-MS method as 3085-2850 and 3700-3360 Ma. In addition, two crystals of zircon were discovered with an age of more than 3800 Ma. According to geo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4f5d2b64b6be3e345a546e5c4d9a6a29
http://dspace.nbuv.gov.ua/handle/123456789/174272
http://dspace.nbuv.gov.ua/handle/123456789/174272
Publikováno v:
Geological Journal. :42-57
The 3.1-3.0 Ga tonalite-trondhjemite-granodiorite rocks of the Middle Dnieper craton were exposed in the provenance of meta-terrigenous rocks of the Hleyuvatka Suite, which forms the upper part of the Krіvоi Rog-Kremenchuk structure. In addition, 3
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa80e01f0bd455726e01d2e150a84d42
https://doi.org/10.30836/igs.1025-6814.2018.2.133457
https://doi.org/10.30836/igs.1025-6814.2018.2.133457
Publikováno v:
Geological Journal. :74-82
Zircons formed at 3.08; 3.17-3.19 and 3.23 Ga were found in metaterrigeneous rocks that occur between horizons of iron-bearing quartzites on the Chertomlyk volcanogenic iron ore deposit. The youngest detrital zircon crystallized at 3.08 Ga signifies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a332c368de1938ba900716157e846709
https://doi.org/10.30836/igs.1025-6814.2014.3.138269
https://doi.org/10.30836/igs.1025-6814.2014.3.138269
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