Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Закарпатський прогин"'
Publikováno v:
Геофізичний журнал; Том 44 № 6 (2022); 24-62
Geofizicheskiy Zhurnal; Vol. 44 No. 6 (2022); 24-62
Геофизический журнал; Том 44 № 6 (2022); 24-62
Geofizicheskiy Zhurnal; Vol. 44 No. 6 (2022); 24-62
Геофизический журнал; Том 44 № 6 (2022); 24-62
The work is devoted to the construction and calculations of a three-dimensional density model of the sedimentary filling of the Carpathian-Pannonian region in order to obtain a more detailed map of the residual gravity field (stripped gravity map). T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::83ea0112b5c91a891182000c7dd301f4
http://journals.uran.ua/geofizicheskiy/article/view/273639
http://journals.uran.ua/geofizicheskiy/article/view/273639
Publikováno v:
Геофізичний журнал; Том 43 № 6 (2021); 120-161
Geofizicheskiy Zhurnal; Vol. 43 No. 6 (2021); 120-161
Геофизический журнал; Том 43 № 6 (2021); 120-161
Geofizicheskiy Zhurnal; Vol. 43 No. 6 (2021); 120-161
Геофизический журнал; Том 43 № 6 (2021); 120-161
An extensive analysis of the available information on the density of themain tectonic elements of the Ukrainian Carpathians is given in connection with the need for further construction of a three-dimensional gravity model. The density was studied bo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::3cd5a7c46ac6c6203fe4e5623277fcdd
http://journals.uran.ua/geofizicheskiy/article/view/251556
http://journals.uran.ua/geofizicheskiy/article/view/251556
Publikováno v:
Geological Journal; № 1 (2020); 34-46
Геологический журнал; № 1 (2020); 34-46
Геологічний журнал; № 1 (2020); 34-46
Геологический журнал; № 1 (2020); 34-46
Геологічний журнал; № 1 (2020); 34-46
In this article, the first Scheme of Neogene volcanism of the western part of Vygorlat-Gutin ridge (Transcarpathian Inner Deep) is presented. The scheme is based on the new comprehensive methology of the stratification and correlation of volcanogenic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::ff0650451706bd76664627eb4f2b2482
http://geojournal.igs-nas.org.ua/article/view/196976
http://geojournal.igs-nas.org.ua/article/view/196976
Autor:
Loktiev, A.A.
Publikováno v:
Geological Journal; № 3 (2019); 45-51
Геологический журнал; № 3 (2019); 45-51
Геологічний журнал; № 3 (2019); 45-51
Геологический журнал; № 3 (2019); 45-51
Геологічний журнал; № 3 (2019); 45-51
The Transcarpathian Neogene depression is surrounded by External Carpathians Panonian basin, east-Slovakian depression and Transilvanian depression. The geologic study within Transcarpathian depression started in XIX century. Active research phase st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::c2be1386f1ab0a783dfee6db37a2c3aa
http://geojournal.igs-nas.org.ua/article/view/177971
http://geojournal.igs-nas.org.ua/article/view/177971
Publikováno v:
Geological Journal; № 1 (2019); 88-108
Геологический журнал; № 1 (2019); 88-108
Геологічний журнал; № 1 (2019); 88-108
Геологический журнал; № 1 (2019); 88-108
Геологічний журнал; № 1 (2019); 88-108
In this article, the first comprehensive stratigraphic scheme of Meso-Cenozoic deposits of Transcarpathian Deep Basement is presented. These deposits spread out in the strip between Pieniny Zone of Carpathians and Pannonian Deep. There are three type
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::a9c8e25df723735a23b603eddc507a63
http://geojournal.igs-nas.org.ua/article/view/159243
http://geojournal.igs-nas.org.ua/article/view/159243
Publikováno v:
ScienceRise; Том 3, № 1 (3) (2014); 42-45
Evolution of views on genesis of natural gases in the depths of Transcarpathian depression is given in the article. Besides another aspect that is mentioned is definition of potential source rocks of oil and gas within the depression by the analysis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=scientific_p::e4b61bb712aae09e0e46be2a1e5788f0
http://journals.uran.ua/sciencerise/article/view/27968
http://journals.uran.ua/sciencerise/article/view/27968