Zobrazeno 1 - 10
of 31
pro vyhledávání: '"A. Ganevich"'
Publikováno v:
Геохімія техногенезу, Vol 6, Iss 34, Pp 71-81 (2021)
The Ingul megablock of the Ukrainian Shield contains a number of endogenous deposits of the sodium-uranium formation, which have been developed for more than 55-60 years. With the exception of the Kirovograd uranium ore region, the deposits of which
Externí odkaz:
https://doaj.org/article/0e0548cceafa4d60becf2827b5d2538d
Publikováno v:
Геохімія техногенезу, Vol 6, Iss 34, Pp 82-89 (2021)
The geological position, composition and genesis of uranium mineralization of ore occurrences on the southwestern slope of the Ukrainian Shield are considered. In the Precambrian basement metamorphic rocks of the Dniester-Bug, Bug and ultrametamorphi
Externí odkaz:
https://doaj.org/article/f2ff10b0a7f64c7e8c2524b61c8bbb83
Publikováno v:
Геохімія техногенезу, Vol 3, Iss 31, Pp 72-78 (2020)
The article discusses the results of comprehensive studies of the integral and differential geodynamics of the Early Proterozoic Novoukrain-skyi granite gneiss dome, which does not have its own petrological, parametric and specialized analogue on the
Externí odkaz:
https://doaj.org/article/69077a4490d1428a864585704ccb7857
Publikováno v:
Geofizicheskiy Zhurnal. 43:80-94
The article discusses the features of the deep and crustal structure of the Golovanevskaya zone, the geochronological sequence of the main stages of its formation. The characteristic of thorium-uranium ore occurrences and deposits is given; and the m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fa955dd8615d85ab035a2571ec005adc
https://doi.org/10.24028/gzh.v43i5.244053
https://doi.org/10.24028/gzh.v43i5.244053
Publikováno v:
Vìsnik Odesʹkogo Nacìonalʹnogo Unìversitetu: Hìmìâ, Vol 17, Iss 4(44), Pp 50-54 (2014)
5,10,15,20-(2-methoxy-3-quinolinyl)porphyrine, which was a mixture of atropisomers, was obtained by condensation of 2-methoxyquinoline-3-carbaldehyde with pyrrole in propionic acid. Quaternization of nitrogen atoms of peripheric substituents in this
Externí odkaz:
https://doaj.org/article/419896b8a7d1446c8fa3c633e9fbec84
Publikováno v:
Геохімія техногенезу, Vol 3, Iss 31, Pp 61-71 (2020)
As a result of urbanization, a new ecological environment has been created with a high concentration of anthropogenic and technogenic factors that affect citizens in large cities and megalopolises. At the same time, a human, as well as biota on the w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fe04b88d8479fd90bc7b31abe158b95e
http://znp.igns.gov.ua/en/1-31-7-geoactive-zones-a-factor-of-influence-on-the-ecology-of-urbanized-territories/
http://znp.igns.gov.ua/en/1-31-7-geoactive-zones-a-factor-of-influence-on-the-ecology-of-urbanized-territories/
Publikováno v:
Геохімія техногенезу, Vol 3, Iss 31, Pp 72-78 (2020)
The article discusses the results of comprehensive studies of the integral and differential geodynamics of the Early Proterozoic Novoukrain-skyi granite gneiss dome, which does not have its own petrological, parametric and specialized analogue on the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9e5bfdd910d63389cde3517b61da168b
http://znp.igns.gov.ua/en/1-31-8-integral-differentiated-palogeodynamics-of-the-new-ukrainian-granite-gneis-dome-of-the-ukrainian-shield/
http://znp.igns.gov.ua/en/1-31-8-integral-differentiated-palogeodynamics-of-the-new-ukrainian-granite-gneis-dome-of-the-ukrainian-shield/
Publikováno v:
Geofizicheskiy Zhurnal. 41:194-209
Most ore occurrences and mineral deposits are known to be located in tectonic fault zones. In this regard, the article analyzes the ore content of regional and local fault zones developed in the megastructures of the Ukrainian shield: Podolsky, Volyn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3aae2f7f3e2184f85e59340dc6ea876e
https://doi.org/10.24028/gzh.0203-3100.v41i4.2019.177388
https://doi.org/10.24028/gzh.0203-3100.v41i4.2019.177388
Publikováno v:
Collected scientific papers Institute of environmental geochemistry. 28:22-32
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::85068a6a0d6a4cf4f54f7b7ba1789fd6
https://doi.org/10.15407/znp2018.28.022
https://doi.org/10.15407/znp2018.28.022
Publikováno v:
Geofizicheskiy Zhurnal; Том 41, № 4 (2019); 194-209
Геофизический журнал; Том 41, № 4 (2019); 194-209
Геофізичний журнал; Том 41, № 4 (2019); 194-209
Геофизический журнал; Том 41, № 4 (2019); 194-209
Геофізичний журнал; Том 41, № 4 (2019); 194-209
Most ore occurrences and mineral deposits are known to be located in tectonic fault zones. In this regard, the article analyzes the ore content of regional and local fault zones developed in the megastructures of the Ukrainian shield: Podolsky, Volyn
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::152b95ca6bc27bf36a31b0a9be14d28a
http://journals.uran.ua/geofizicheskiy/article/view/177388
http://journals.uran.ua/geofizicheskiy/article/view/177388