from 01.01.2019 until now
Aprelevka Branch of the All-Russian Research Geological Oil Institute
from 01.01.2019 until now
Moscow, Russian Federation
Novosibirsk, Russian Federation
Moscow, Russian Federation
Russian Federation
VAC 1.6 Науки о Земле и окружающей среде
UDK 551.762 Юра (180-135 млн. лет)
UDK 551.761 Триас (220-180 млн. лет) Орогения: Полисадская
UDK 551.7 Историческая геология. Стратиграфия
UDK 55 Геология. Геологические и геофизические науки
UDK 550.34 Сейсмология
UDK 550.383 Главное магнитное поле Земли
GRNTI 38.29 Стратиграфия
GRNTI 38.31 Палеонтология
GRNTI 38.21 Региональная геология
GRNTI 37.01 Общие вопросы геофизики
GRNTI 37.15 Геомагнетизм и высокие слои атмосферы
GRNTI 37.25 Океанология
GRNTI 37.31 Физика Земли
GRNTI 38.01 Общие вопросы геологии
GRNTI 36.00 ГЕОДЕЗИЯ. КАРТОГРАФИЯ
GRNTI 37.00 ГЕОФИЗИКА
GRNTI 38.00 ГЕОЛОГИЯ
GRNTI 39.00 ГЕОГРАФИЯ
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OKSO 05.03.01 Геология
OKSO 05.00.00 Науки о Земле
BBK 263 Геологические науки
BBK 26 Науки о Земле
TBK 63 Науки о Земле. Экология
BISAC SCI091000 Earth Sciences / Sedimentology & Stratigraphy
BISAC SCI SCIENCE
The section of Cape Airkat on the western shore of the Anabar Bay has been a reference section for the study of the Triassic and Jurassic in the Anabar region, but its subdivision is still a subject of controversy. A detailed lithological and paleontological characteristic of the section is given. Based on the existing data on the genesis of the Triassic-Jurassic boundary deposits, the boundaries of local stratigraphic units were revised, and for the first time the Bulunkan Formation was identified in the interval of the section, which was previously considered the basal part of the “Zimnyaya Formation”. A new Laptevomorskaya Formation was identified in place of the Zimnyaya Formation, which was previously found to be widespread in western Siberia. Its lower boundary is drawn at the base of a marking horizon of clays of coastal-marine genesis. The Hettangian age of the lower part of the Laptevomorskaya Formation was determined on the basis of bivalves. The Triassic-Jurassic boundary is proposed to be conditionally combined with the base of the Laptevomorskaya Formation. Key species of Rhaetian and Lower Hettangian bivalves and brachiopods are figured.
Rhaetian, Hettangian, stratigraphy, bivalves, Siberia
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