MOLAR TOOTH STRUCTURES IN CALCAREOUS NODULES, EARLY NEOPROTEROZOIC BUROVAYA FORMATION, TURUKHANSK REGION, SIBERIA

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dc.contributor.author Pope M.C.
dc.contributor.author Bartley J.K.
dc.contributor.author Knoll A.H.
dc.contributor.author Petrov P.Y.
dc.date.accessioned 2022-02-17T11:03:51Z
dc.date.available 2022-02-17T11:03:51Z
dc.date.issued 2003
dc.identifier https://elibrary.ru/item.asp?id=13441318
dc.identifier.citation Sedimentary Geology, 2003, 158, 3-4, 235-248
dc.identifier.issn 0037-0738
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/35488
dc.description.abstract Molar tooth structures are abundant in large (1-2 m diameter) carbonate nodules within fine-grained, subtidal carbonates of the early Neoproterozoic (lower Upper Riphean) Burovaya Formation along the Sukhaya Tunguska River, Turukhansk Uplift, northwestern Siberia. Although molar tooth structures are regionally abundant in this unit, here they occur only within the nodules. Stable isotopic compositions of molar-tooth-filling dolomicrospar cements and of thinly bedded dolomicrite within and surrounding the nodules are indistinguishable from one another. The carbon isotopic compositions (mean δ
dc.subject Molar tooth structures
dc.subject Carbonate
dc.subject Stable isotopes
dc.subject Neoproterozoic
dc.title MOLAR TOOTH STRUCTURES IN CALCAREOUS NODULES, EARLY NEOPROTEROZOIC BUROVAYA FORMATION, TURUKHANSK REGION, SIBERIA
dc.type Статья
dc.subject.age Precambrian::Proterozoic::Mesoproterozoic
dc.subject.age Precambrian::Proterozoic::Neoproterozoic
dc.subject.age Докембрий::Протерозой::Неопротерозойская ru
dc.subject.age Докембрий::Протерозой::Мезопротерозойская ru


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