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

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.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.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.subject	Molar tooth structures
dc.subject	Carbonate
dc.subject	Stable isotopes
dc.subject	Neoproterozoic
dc.subject.age	Precambrian::Proterozoic::Mesoproterozoic
dc.subject.age	Precambrian::Proterozoic::Neoproterozoic
dc.title	MOLAR TOOTH STRUCTURES IN CALCAREOUS NODULES, EARLY NEOPROTEROZOIC BUROVAYA FORMATION, TURUKHANSK REGION, SIBERIA
dc.type	Статья

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