Neogene river system of the Shatsky Swell in the Black Seaстатья
Информация о цитировании статьи получена из
Web of Science ,
Scopus
Статья опубликована в журнале из списка Web of Science и/или Scopus
Дата последнего поиска статьи во внешних источниках: 18 июля 2013 г.
Авторы:
Afanasenkov A.P.a ,
Nikishin A.M.b ,
Obukhov A.N.a
Журнал:
Doklady Earth Sciences
Том:
403
Номер:
5
Год издания:
2005
Издательство:
Maik Nauka/Interperiodica Publishing
Местоположение издательства:
Russian Federation
Первая страница:
677
Последняя страница:
680
Аннотация:
The geological structure of the eastern Black Sea region has been relatively well studied by a number of researchers. Two buried Neogene erosional channels have been established in the sotheastern part of the Tuapse Trough. The majority of seismic materials were subjected to so-called "PreStackDepthMigration" processing. The seismic depth profiles based on the special processing method mentioned above, along with other available records and materials of field studies in the eastern Black Sea region, served as the basis for this work. Copright В© 2005 by Pleiades Publishing, Inc.
Добавил в систему:
Никишин Анатолий Михайлович