The isotopic–geochronological age of trap formation rocks in the sedimentary section of the Baikit anteclise
- 作者: Alekseeva K.S.1, Popova L.P.1, Postnikov A.V.1, Postnikova O.V.1
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隶属关系:
- Gubkin Russian State University of Oil and Gas
- 期: 卷 470, 编号 2 (2016)
- 页面: 1014-1018
- 栏目: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/188974
- DOI: https://doi.org/10.1134/S1028334X16100196
- ID: 188974
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详细
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.
作者简介
K. Alekseeva
Gubkin Russian State University of Oil and Gas
Email: olgapostnikova@yandex.ru
俄罗斯联邦, Leninskii pr. 65, Moscow, 119991
L. Popova
Gubkin Russian State University of Oil and Gas
Email: olgapostnikova@yandex.ru
俄罗斯联邦, Leninskii pr. 65, Moscow, 119991
A. Postnikov
Gubkin Russian State University of Oil and Gas
Email: olgapostnikova@yandex.ru
俄罗斯联邦, Leninskii pr. 65, Moscow, 119991
O. Postnikova
Gubkin Russian State University of Oil and Gas
编辑信件的主要联系方式.
Email: olgapostnikova@yandex.ru
俄罗斯联邦, Leninskii pr. 65, Moscow, 119991
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