THE LOWER BOUNDARY OF THE TRIASSIC AND ITS CORRELATION IN MARINE SEDIMENTS: PAPER 1. BOUNDARY SECTIONS OF THE TETHYS

dc.contributor.author	Shevyrev A.A.
dc.date.accessioned	2021-01-11T07:57:16Z
dc.date.available	2021-01-11T07:57:16Z
dc.date.issued	1999
dc.identifier	https://elibrary.ru/item.asp?id=13316217
dc.identifier.citation	Stratigraphy and Geological Correlation, 1999, , 2, 116-129
dc.identifier.issn	0869-5938
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/22660
dc.description.abstract	In the Tethys region, the Triassic starts with the ammonite Otoceras woodwardi Zone accepted as basal in this system more than a hundred years ago. The boundary layers in Ciscaucasia, Iran, western Pakistan, Kashmir, central Himalayas, southern China, and Thailand are considered. The uppermost Permian deposits bearing Paratirolites or Pseudotirolites are well represented in the Paleotethys sections. In the Neotethys sections, the Otoceras genus often appears along with the Ophiceras genus and in association with conodonts Hindeodus parvis.
dc.subject	Triassic	en
dc.title	THE LOWER BOUNDARY OF THE TRIASSIC AND ITS CORRELATION IN MARINE SEDIMENTS: PAPER 1. BOUNDARY SECTIONS OF THE TETHYS
dc.type	Статья
dc.subject.age	Mesozoic::Triassic	en
dc.subject.age	Мезозой::Триасовая	ru

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