THE FIRST JOINT FIND OF CONIACIAN-SANTONIAN RADIOLARIANS AND PLANKTONIC FORAMINIFERS IN WESTERN KAMCHATKA

dc.contributor.authorVishnevskaya V.S.
dc.contributor.authorBasov I.A.
dc.contributor.authorKurilov D.V.
dc.date.accessioned2024-10-23T07:16:04Z
dc.date.available2024-10-23T07:16:04Z
dc.date.issued2006
dc.description.abstractRadiolarians and inoceramids in Santonian–early Campanian neritic facies of northwestern Kamchatka were known long ago. The radiolarian assemblage, which includes 25 species, originates from carbonate concretions in the siliciclastic rocks (siltstones and sandstones) of the lower subformation of the Bystraya Formation (Talovka Group) developed in the lower reaches of the eponymous river. This assemblage is represented by species known only from the Russian Platform and California in a 2 : 1 proportion.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13512625
dc.identifier.citationDoklady Earth Sciences, 2006, 409, 5, 701-705
dc.identifier.doi10.1134/S1028334X06050047
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46170
dc.subjectSantonian
dc.subjectConiacian
dc.subject.ageMesozoic::Cretaceous::Upper::Santonian
dc.subject.ageМезозой::Меловая::Верхний::Сантонский
dc.subject.ageMesozoic::Cretaceous::Upper::Coniacian
dc.subject.ageМезозой::Меловая::Верхний::Коньякский
dc.titleTHE FIRST JOINT FIND OF CONIACIAN-SANTONIAN RADIOLARIANS AND PLANKTONIC FORAMINIFERS IN WESTERN KAMCHATKA
dc.typeСтатья

Файлы

Оригинальный пакет

Показано 1 - 1 из 1
Загрузка...
Изображение-миниатюра
Имя:
Vish_06.pdf
Размер:
269.62 KB
Формат:
Adobe Portable Document Format

Коллекции