THE LOWER BOUNDARY OF THE TRIASSIC AND ITS CORRELATION IN MARINE SEDIMENTS: PAPER 1. BOUNDARY SECTIONS OF THE TETHYS
- DSpace Home
- →
- Геология России
- →
- ELibrary
- →
- View Item
JavaScript is disabled for your browser. Some features of this site may not work without it.
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 |
Files in this item
Files | Size | Format | View |
---|---|---|---|
There are no files associated with this item. |
This item appears in the following Collection(s)
-
ELibrary
Метаданные публикаций с сайта https://www.elibrary.ru