Enviar artigo por via de e-mail The isotopic–geochronological age of trap formation rocks in the sedimentary section of the Baikit anteclise
- Autores: Alekseeva K.S.1, Popova L.P.1, Postnikov A.V.1, Postnikova O.V.1
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Afiliações:
- Gubkin Russian State University of Oil and Gas
- Edição: Volume 470, Nº 2 (2016)
- Páginas: 1014-1018
- Seção: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/188974
- DOI: https://doi.org/10.1134/S1028334X16100196
- ID: 188974
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Resumo
The Lower Cambrian Usol’e Formation in the Kamov arch of the Baikit anteclise includes stratiform intrusions confined to several levels. According to isotopic‒geochronological investigations, the age of stratiform intrusions composed of olivine dolerites is estimated to be 256.0 ± 3.2 Ma.
Sobre autores
K. Alekseeva
Gubkin Russian State University of Oil and Gas
Email: olgapostnikova@yandex.ru
Rússia, Leninskii pr. 65, Moscow, 119991
L. Popova
Gubkin Russian State University of Oil and Gas
Email: olgapostnikova@yandex.ru
Rússia, Leninskii pr. 65, Moscow, 119991
A. Postnikov
Gubkin Russian State University of Oil and Gas
Email: olgapostnikova@yandex.ru
Rússia, Leninskii pr. 65, Moscow, 119991
O. Postnikova
Gubkin Russian State University of Oil and Gas
Autor responsável pela correspondência
Email: olgapostnikova@yandex.ru
Rússia, Leninskii pr. 65, Moscow, 119991
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