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Late Jurassic carbonate buildups in the northern part of the Shatsky ridge, Black Seaстатья
Информация о цитировании статьи получена из
Scopus
Дата последнего поиска статьи во внешних источниках: 28 мая 2015 г.
- Авторы: Afanasenkov A.P., Nikishin A.M., Obukhov A.N.
- Журнал: Doklady Akademii nauk SSSR
- Том: 403
- Номер: 2
- Год издания: 2005
- Издательство: Akademiia Nauk Sssr
- Местоположение издательства: Russian Federation
- Первая страница: 216
- Последняя страница: 219
- Аннотация: For the first time showed is the scale of carbonate buildups system spreading and its tectonic position with account of analysis of all other available profiles and the conducted field investigations around the Black Sea region. It is concluded that in the Callovian-Late Jurassic period in the Shatsky ridge domain sedimentary mantle was forming, but this domain was differentiated. In the northern part of the Shatsky ridge after a hypothetical Callovian rifting phase, deep Late Jurassic submerging occurred (up to 1.5-2 km), on which background the system of rift-type carbonate buildups surrounded by zones of non-compensated carbonate-clay sediment accumulation was formed. In the South-Adler zone in the Callovian-Late Jurassic the South-Adler carbonate shelf platform was formed; along its northern age, apparently, the reef belt was formed, which on the ground is known in Abkhasia and Adler region (the Akhtzu zone).
- Добавил в систему: Никишин Анатолий Михайлович