Zobrazeno 1 - 10
of 165
pro vyhledávání: '"A.A. Svitoch"'
Publikováno v:
Quaternary International. :93-107
Two Pleistocene sections in the middle reaches of the Volga River – Spasskoe and Yagodnoe – have been described in details and analyzed, small mammal remains being recovered and identified. The fauna includes remains of open landscape species: Eo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::93731bff243da59b0243784f25a65f0d
https://doi.org/10.1016/j.quaint.2020.12.001
https://doi.org/10.1016/j.quaint.2020.12.001
Autor:
A.A. Svitoch, R.R. Makshaev
Publikováno v:
Quaternary International. 540:78-96
Pleistocene key sections of the Northern Caspian Lowland are characterized by the incompleteness of the geological record, which is presented in depositional breaks, their duration, causes, and types. Depositional breaks occurred in all periods of th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8549d355943341fb090f58a1d4d52bca
https://doi.org/10.1016/j.quaint.2019.04.030
https://doi.org/10.1016/j.quaint.2019.04.030
Publikováno v:
Limnology and Freshwater Biology. :531-532
Early Khvalynian basin was one of the largest in the history of the Caspian Sea during the Pleistocene. Six lithofacies (LF1-LF6) with two subfacies (LF2a-LF2b) are recognized in lower khvalynian deposits in the Lower Volga Region (the Northern Caspi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::803801e940ebe639f2377e40664a9396
https://doi.org/10.31951/2658-3518-2020-a-4-531
https://doi.org/10.31951/2658-3518-2020-a-4-531
Autor:
R.R. Makshaev, A.A. Svitoch
Publikováno v:
Quaternary International. 409:44-49
The chocolate clays commonly comprise a part of the Lower Khvalynian sequence in the northern Caspian Lowland and in the Volga region. The mode of occurrence varies from continuous to patchy mosaic. All the clay deposits are confined to Pre-Khvalynia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f9220bb3e14665575226d6d0ad30016
https://doi.org/10.1016/j.quaint.2015.07.018
https://doi.org/10.1016/j.quaint.2015.07.018
Autor:
N.I. Tertychniy, A. A. Starikova, R.R. Makshaev, S. B. Chernov, Tamara Yanina, A.A. Svitoch, Kh. A. Arslanov, Andrey L. Chepalyga, Fedor Maksimov
Publikováno v:
Quaternary International. 409:81-87
During the second half of the late Pleistocene, the Caspian experienced repeated transgressions (Early and Late Khvalynian) and regressions (Enotaevsk and Mangyshlak) with an oscillation amplitude of 120 e150 m. The question about the age of the Khva
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b960b478c601f4985e8e681f2771a6a7
https://doi.org/10.1016/j.quaint.2015.05.067
https://doi.org/10.1016/j.quaint.2015.05.067
Publikováno v:
Quaternary International. 409:8-15
Marine Holocene deposits of the coast of Iran are represented by the Upper Khvalinian and New Caspian beds. Upper Khvalinian sediments are faunistically barren, whereas the New Caspian beds contain abundant fossil molluscs that allow subdivision into
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9953a6416bac271d696f83eeb1185523
https://doi.org/10.1016/j.quaint.2014.05.047
https://doi.org/10.1016/j.quaint.2014.05.047
Publikováno v:
Doklady Earth Sciences. 459:1623-1626
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1af3adaa3f36b467ef641fa212dbec77
https://doi.org/10.1134/s1028334x14120265
https://doi.org/10.1134/s1028334x14120265
Publikováno v:
Doklady Earth Sciences. 451:843-848
The Iranian coast of the Caspian Sea is an element of the South Caspian Depression, which represents a spacious plain with a subtropical climate bordered in the south by the Elburs mountainous system. Its west� ern, central, and eastern parts bear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::58af1779a9cc59d295d5b38b47812fe1
https://doi.org/10.1134/s1028334x13080060
https://doi.org/10.1134/s1028334x13080060
Autor:
G.V. Rusakov, A.A. Svitoch, K. Groenesteijn, Salomon B. Kroonenberg, A. Veldkamp, Irina Overeem
Publikováno v:
Sedimentary Geology, 159(3-4-2017), 133-157. Elsevier
Sedimentary Geology, 159, 133-157
Sedimentary Geology 159 (2003)
Sedimentary Geology, 159, 133-157
Sedimentary Geology 159 (2003)
The Volga delta differs from all other major deltas in the world by its extremely gentle onshore and offshore gradient (similar to 5 cm/km) and by being affected by the rapid sea-level changes of the Caspian Sea, at rates up to a hundred times the gl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::972b275da7bd0687d6809331275cd663
https://doi.org/10.1016/s0037-0738(02)00256-7
https://doi.org/10.1016/s0037-0738(02)00256-7
Autor:
A.A. Svitoch
Publikováno v:
The Handbook of Environmental Chemistry ISBN: 9783540882763
The Aral Sea basin formed as a result of joint action of tectonic subsidence and processes of arid denudation. The basin itself features rather irregular bottom topography, with depressions divided by an elongated elevation trending from north to sou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2a5913059e22c00bef3be0a5c5c2890d
https://doi.org/10.1007/698_2009_7
https://doi.org/10.1007/698_2009_7
