The isotopic–geochronological age of trap formation rocks in the sedimentary section of the Baikit anteclise


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

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

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2016