IDENTIFYING UPPER MIOCENE – LOWER PLIOCENE LACUSTRINE SEDIMENTS IN DRY TUNKA BASIN OF THE BAIKAL RIFT ZONE
We present results of lithogeochemical, diatomic and palynological studies of sediments from the Tunka-13 well that was drilled in the southeastern part of dry Tunka basin in the Baikal rift zone. At the base of the section, there is an eroded basaltic flow of 16–15 Ma. From lithogeochemical signatu...
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| Principais autores: | , , , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
2020-06-01
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| coleção: | Геодинамика и тектонофизика |
| Assuntos: | |
| Acesso em linha: | https://www.gt-crust.ru/jour/article/view/1031 |
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