ELEMENTARY STRATIGRAPHIC UNITS
| dc.contributor.author | Afanasev S.L. | |
| dc.date.accessioned | 2020-12-23T08:31:35Z | |
| dc.date.available | 2020-12-23T08:31:35Z | |
| dc.date.issued | 1997 | |
| dc.description.abstract | It has been established that every tenth bed of the Upper Cretaceous-Danian flysch deposits can be traced along the southern slope of the Greater Caucasus over a distance of 1035 km. This allowed 196 synchronous markers to be established in this region. Their synchronism is based on a relative number of cyclites and confirmed by paleontologic data. The formation time of one global stratigraphic unit is assumed to average 22 ± 9 k.y. | |
| dc.identifier | https://elibrary.ru/item.asp?id=13265026 | |
| dc.identifier.citation | Stratigraphy and Geological Correlation, 1997, , 5, 501-508 | |
| dc.identifier.issn | 0869-5938 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/21180 | |
| dc.subject | Cretaceous | en |
| dc.subject.age | Кайнозой::Палеоген::Палеоцен::Датский | ru |
| dc.title | ELEMENTARY STRATIGRAPHIC UNITS | |
| dc.type | Статья |