|
ИСТИНА |
Войти в систему Регистрация |
ИПМех РАН |
||
Oligocene to Neogene paleogeography and depositional environments of the Euxinian part of Paratethys in Crimean – Caucasian junctionстатья
Статья опубликована в высокорейтинговом журнале
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: 3 июля 2019 г.
- Авторы: Popov S.V., Rostovtseva Yu V., Pinchukc T.N., Patina I.S., Goncharova I.A.
- Журнал: Marine and Petroleum Geology
- Том: 103
- Год издания: 2019
- Издательство: Elsevier BV
- Местоположение издательства: Netherlands
- Первая страница: 163
- Последняя страница: 175
- DOI: 10.1016/j.marpetgeo.2019.02.019
- Аннотация: Paleogeography and depositional environments in the zone of junction of the Crimea and the Greater Caucasus, as well as adjacent areas of the West Kuban Basin, the Sea of Azov and the Western Ciscaucasia are described based on the results of drilling works, seismic studies and multidisciplinary research. Paleogeographic maps are compiled for the early Oligocene, middle Miocene (Karaganian and early Sarmatian) and late Miocene (late Maeotian and early Pontian). The maps represented show gradual sediment filling of the deep West Kuban trough during the Maikopian and middle Miocene, and its gradual closure in the Kerch-Taman area. The deepwater connection of this trough with the Black Sea basin through the Sorokin trough had been closed by the mid- Sarmatian. The entire Kerch-Taman region became shallow by the end of the Maeotian. Significant sea level falls occurred at the end of the Tarkhanian and Sarmatian as well as in the middle of the Pontian. Large erosion channels from these times are traced on the geological and seismic profiles of the northern Scythian shelf.
- Добавил в систему: Ростовцева Юлиана Валерьевна