Email this article The isotopic–geochronological age of trap formation rocks in the sedimentary section of the Baikit anteclise
- Authors: Alekseeva K.S.1, Popova L.P.1, Postnikov A.V.1, Postnikova O.V.1
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Affiliations:
- Gubkin Russian State University of Oil and Gas
- Issue: Vol 470, No 2 (2016)
- Pages: 1014-1018
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/188974
- DOI: https://doi.org/10.1134/S1028334X16100196
- ID: 188974
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Abstract
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.
About the authors
K. S. Alekseeva
Gubkin Russian State University of Oil and Gas
Email: olgapostnikova@yandex.ru
Russian Federation, Leninskii pr. 65, Moscow, 119991
L. P. Popova
Gubkin Russian State University of Oil and Gas
Email: olgapostnikova@yandex.ru
Russian Federation, Leninskii pr. 65, Moscow, 119991
A. V. Postnikov
Gubkin Russian State University of Oil and Gas
Email: olgapostnikova@yandex.ru
Russian Federation, Leninskii pr. 65, Moscow, 119991
O. V. Postnikova
Gubkin Russian State University of Oil and Gas
Author for correspondence.
Email: olgapostnikova@yandex.ru
Russian Federation, Leninskii pr. 65, Moscow, 119991
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