Zobrazeno 1 - 10
of 106
pro vyhledávání: '"N. I. Zaporozhets"'
Autor:
S. V. Popov, G. N. Aleksandrova, A. A. Voronina, N. I. Zaporozhets, L. A. Golovina, K. P. Koiava
Publikováno v:
Stratigraphy and Geological Correlation. 30:408-430
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e3777a5979f8e986ced11d161522cc0a
https://doi.org/10.1134/s0869593822050057
https://doi.org/10.1134/s0869593822050057
Autor:
V. N. Beniamovsky, A. S. Stolyarov, N. I. Zaporozhets, Sergey V. Popov, A. B. Bogachkin, M. A. Akhmetiev, V. A. Musatov, A. S. Zastrozhnov
Publikováno v:
Stratigraphy and Geological Correlation. 27:442-474
This work presents the results of the integrated study of the sequence of Oligocene (Maikop) and underlying Eocene deposits uncovered in borehole 768 (362 m). This section can be regarded as the reference one as for Northern Ergeni, as for the entire
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a8f45af7a0dcfa9b3755665a35fc3756
https://doi.org/10.1134/s0869593819040063
https://doi.org/10.1134/s0869593819040063
Autor:
V. N. Benyamovsky, A. B. Bogachkin, A. S. Stolyarov, Sergey V. Popov, V. A. Musatov, A. S. Zastrozhnov, M. A. Akhmetiev, N. I. Zaporozhets
Publikováno v:
Стратиграфия. 27:59-92
The section of well 768, depth 362 m, which opened the Eocene and Maikopian deposits is comprehensively studied and can serve as a reference one for both the Northern Ergeny and the entire northern part of Paratethys. The data on lithology, mollusks,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f7a93d5aad5914a6103074ce57319074
https://doi.org/10.31857/s0869-592x27459-92
https://doi.org/10.31857/s0869-592x27459-92
Autor:
Wout Krijgsman, А. S. Stolyarov, M. A. Akhmet’ev, I. P. Tabachnikova, А. van der Boon, J. Krhovsky, Sergey V. Popov, A. F. Bannikov, T. N. Pinchuk, E. K. Sychevskaya, N. I. Zaporozhets
Publikováno v:
Стратиграфия. 27:70-92
Belaya River Section of Maikop deposits is the closest to the Maikop town, typical for Western and Central Ciscaucasus, well outcropped and studied and should be considered as a type section for the Maikop Group. Here it is possible to observe a cont
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eb075690694e0f447697d61debccf723
https://doi.org/10.31857/s0869-592x27370-92
https://doi.org/10.31857/s0869-592x27370-92
Publikováno v:
Stratigraphy and Geological Correlation. 27:118-132
The Eocene interval of the section in the Belaya River valley is continuously exposed and is represented (from the bottom up) by green clays of the Cherkessk Formation, the marl–clayey member of the Keresta Formation, bituminous marls of the Kuma F
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::943386d78967219b67c796c1cfb88f37
https://doi.org/10.1134/s0869593819010052
https://doi.org/10.1134/s0869593819010052
Autor:
N. I. Zaporozhets, M. A. Akhmetiev
Publikováno v:
Stratigraphy and Geological Correlation. 25:638-658
A stratotypical section of the Oligocene–Lower Miocene Maikop Group in the valley of the Belaya River above the city of Maikop was studied using a complex paleobotanical method. The hydrological regime of marine basin was specified, especially for
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ab7ecda5941988fca650d6a43590e8f
https://doi.org/10.1134/s0869593817060089
https://doi.org/10.1134/s0869593817060089
Publikováno v:
Doklady Earth Sciences. 473:273-276
The Eocene and Oligocene transition sections (Priabonian–Rupelian) of the Aral–Turgai, West Siberian, Volga–Don, and Crimea–Caucasus regions have been studied in detail [1], and the global biospheric crisis events have been estimated at the t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43f5d25902ce46769107af42636b1c49
https://doi.org/10.1134/s1028334x17030199
https://doi.org/10.1134/s1028334x17030199
Autor:
M. A. Akhmetiev, N. I. Zaporozhets
Publikováno v:
Stratigraphy and Geological Correlation. 25:229-239
Paleobotanical evidence for the climate-forming significance of marine currents in the Early Paleogene of the Arctic is reported. It is based on the analysis of mega- and microfossil plant assemblages derived from the outcrops located along the Arcti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b42a6e49959a208453258caa180d32fa
https://doi.org/10.1134/s0869593817020022
https://doi.org/10.1134/s0869593817020022
Autor:
N. I. Zaporozhets, M. A. Akhmetiev
Publikováno v:
Stratigraphy and Geological Correlation. 23:326-350
The analysis of organic-walled phytoplankton, pollen, and spores in sections of the Solenovian Horizon (second half of the lower Oligocene) in the Western Carpathians, Crimea-Caucasus region, and Scythian and Turan plates revealed that facies of a mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8aa5c0f1f791be8982f0d5bf32675c60
https://doi.org/10.1134/s0869593815030077
https://doi.org/10.1134/s0869593815030077
Autor:
Anatoly M. Nikishin, E. V. Rubtsova, P.A. Fokin, N. I. Zaporozhets, L. F. Kopaevich, A. V. Mityukov, O. A. Khlebnikova
Publikováno v:
Moscow University Geology Bulletin. 69:399-409
The lower part of the Maykop Group sediments of the Crimea-Caucasus region were studied. Available outcrops of every structure-facies zone were examined and the sandstone composition was determined in thin sections: as a result five main lithologies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f5a7974b03a562713f6b8ce4fa6343db
https://doi.org/10.3103/s0145875214060076
https://doi.org/10.3103/s0145875214060076