Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Nikolay V Esin"'
Publikováno v:
Hydrosphere Еcology (Экология гидросферы). :28-39
One of the important unsolved problems related to the evolution of living conditions on Earth is the mechanism of the rapid transformation of the Black Sea from a shallow lake-type sea into a deep-water basin, the earth's crust in the central part of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a127f3fe783117b554a86301ae1bb62
https://doi.org/10.33624/2587-9367-2021-1(6)-28-39
https://doi.org/10.33624/2587-9367-2021-1(6)-28-39
Publikováno v:
Hydrosphere Еcology (Экология гидросферы). :1-9
The article presents a solution to an equation describing the processes of filling depressions with water in the relief of formation and ancient transgressive seas. A model has been developed for the course of the sea level during the creation of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53533c9ca0825ff2e93aead7be071fa8
https://doi.org/10.33624/2587-9367-2020-1(5)-1-9
https://doi.org/10.33624/2587-9367-2020-1(5)-1-9
Publikováno v:
Hydrosphere Еcology (Экология гидросферы). :1-7
The article calculates the freshwater balance of the ancient Black and Caspian seas and estimates the volume of water flowing from the Black Sea to the Mediterranean during the melting of glaciers. It is shown that during this period up to 855 km3/ye
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ec8483b79bacd80094f974c9a3ff00bc
https://doi.org/10.33624/2587-9367-2019-2(4)-1-7
https://doi.org/10.33624/2587-9367-2019-2(4)-1-7
Publikováno v:
Hydrosphere Еcology (Экология гидросферы). :13-23
The basis of the theory of evolution of transgressive the Akchagyl Sea is based on the hypothesis that the transgression was created by water coming from an as yet unidentified ocean. This causes some doubt due to the fact that in the Akchagyl time t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08543b4f8ceced74a7759d1a17f91b11
https://doi.org/10.33624/2587-9367-2019-1(3)-13-23
https://doi.org/10.33624/2587-9367-2019-1(3)-13-23
Publikováno v:
Quaternary International. 465:54-62
This paper aims to develop a theoretical hydromechanical model designed to explain slow motion of thin sediment suspension layer over the Black Sea abyssal plain. The suspension flows are regarded as a new lateral deep sea sediment transport mechanis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9d2da11d657378d9bcd1ae6cfe020c04
https://doi.org/10.1016/j.quaint.2017.07.025
https://doi.org/10.1016/j.quaint.2017.07.025
Publikováno v:
Quaternary International. 465:46-53
A possible mechanism leading to the transformation of the Paratethys seas (i.e., the Sarmatian Sea-Lake, Meotian Sea, Pontian Sea-Lake, etc.) is here proposed. The time period from the formation of the closed Sarmatian Sea-Lake to the present is also
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bddd9e876fc9ffff06697114c456c749
https://doi.org/10.1016/j.quaint.2016.06.019
https://doi.org/10.1016/j.quaint.2016.06.019
Autor:
Nikolay V. Esin, Nikolay I. Esin
Publikováno v:
Hydrosphere Еcology (Экология гидросферы). :7-14
In the article the ancient geological processes of transporting a huge volume of water (up to 2500 km3/year), whereby the Paratethys Sea and the Manych, Bosporus and Dardanelles straits was formed, are regarded as deterministic physical processes. In
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2b7129ed879d95886c744fbac3e13e09
https://doi.org/10.33624/2587-9367-2018-1(2)-7-14
https://doi.org/10.33624/2587-9367-2018-1(2)-7-14
Publikováno v:
Quaternary International. 409:33-38
The origin of the bottom counterflow in Bosphorus Strait during the early Holocene, its temporal development and the Black Sea filling by the Mediterranean salt water is discussed in this paper. At 10 ka, the depth of the strait was 10 m, the velocit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bf196ac25ff928c98043f799c92ddea6
https://doi.org/10.1016/j.quaint.2015.05.011
https://doi.org/10.1016/j.quaint.2015.05.011
Autor:
Nikolay V. Esin, Nikolay I. Esin
Publikováno v:
Quaternary International. 345:32-47
A mathematical model of the Black Sea level change for the last 20,000 years is presented in this paper, based on the equations of viscous incompressible fluid motion according to Navier–Stokes, Sen-Venans, and the equation of water balance in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bbde50bf730cc9ad056dd94dbdd2936b
https://doi.org/10.1016/j.quaint.2014.05.026
https://doi.org/10.1016/j.quaint.2014.05.026
Publikováno v:
Quaternary International. 225:180-190
Although the Late Pleistocene–Holocene fluctuations in the Black Sea have been studied over many years, no overall picture of this difficult natural phenomenon has as yet been developed and described. Moreover, in the literature, many researchers h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c25e046ea591dcac39b0afe2e90b1c05
https://doi.org/10.1016/j.quaint.2009.11.014
https://doi.org/10.1016/j.quaint.2009.11.014