40AR-39AR AGE OF SIBERIAN BASALTIC VOLCANISM
- 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 | Venkatesan T.R. | |
dc.contributor.author | Kumar A. | |
dc.contributor.author | Gopalan K. | |
dc.contributor.author | Al'mukhamedov A.I. | |
dc.date.accessioned | 2020-12-24T03:35:20Z | |
dc.date.available | 2020-12-24T03:35:20Z | |
dc.date.issued | 1997 | |
dc.identifier | https://elibrary.ru/item.asp?id=13268843 | |
dc.identifier.citation | Chemical Geology, 1997, , 3, 303-310 | |
dc.identifier.issn | 0009-2541 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/21185 | |
dc.description.abstract | Five of six samples representing the entire stratigraphic sequence (∼3700 m thick) of basaltic flows in the Noril'sk section in the northwestern part of Siberian flood basalt province, Russia yield 40Ar–39Ar plateau ages between 248.3±1.7 Ma and 246.9±2.5 Ma relative to an age of 520.4 Ma for the hornblende standard, MMhb-1. These results clarify some discrepancies in existing data and confirm that eruption of the bulk of Siberian basalts was close to 248 Ma and possibly lasted less than 2 Ma. Although the violence of this volcanism may have caused the massive extinctions at the Permo–Triassic boundary, the onset of changes across this boundary seems to have been distinctly earlier. | |
dc.subject | Triassic | en |
dc.subject | Permian | |
dc.title | 40AR-39AR AGE OF SIBERIAN BASALTIC VOLCANISM | |
dc.type | Статья | |
dc.subject.age | Mesozoic::Triassic | en |
dc.subject.age | Paleozoic::Permian | |
dc.subject.age | Мезозой::Триасовая | ru |
dc.subject.age | Палеозой::Пермская | 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