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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Main Authors: A. Hassan, S. V. Rasskazov, I. S. Chuvashova, T. A. Yasnygina, L. A. Titova, N. V. Kulagina, M. V. Usoltseva
Formato: Artigo
Idioma:Inglês
Publicado em: Institute of the Earth's crust, Siberian Branch of RAS 2020-06-01
Colecção:Geodinamika i Tektonofizika
Assuntos:
baikal
tunka basin
sediments
volcanism
miocene
pliocene
stratigraphy
lithogeochemistry
diatom analysis
palynological analysis
Acesso em linha:https://www.gt-crust.ru/jour/article/view/1031
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