The First Precise Data on the Age of Charoite Mineralization (Eastern Siberia, Russia)
- 作者: Ivanov A.V.1, Gorovoy V.A.1, Gladkochub D.P.1, Shevelev A.S.1, Vladykin N.V.2
-
隶属关系:
- Institute of the Earth’s Crust, Siberian Branch
- Vinogradov Institute of Geochemistry, Siberian Branch
- 期: 卷 478, 编号 2 (2018)
- 页面: 179-182
- 栏目: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/192182
- DOI: https://doi.org/10.1134/S1028334X18020241
- ID: 192182
如何引用文章
详细
Charoite is a unique mineral and a rock of the same name. It is known from the only deposit in the world at the contact with Early Cretaceous syenite and other alkaline rocks of the Malyi Murun massif. The data on 40Ar/39Ar dating of tinaksite, tokkoite, and frankamenite associated with charoite are reported in this paper. All these minerals, except for frankamenite, have shown clear plateau ages overlapping with each other within the analytical errors. The weighted mean of the plateau ages of tinaksite, tokkoite, and microcline is 135.86 ± 0.26 Ma. Considering that these minerals are syngenetic to charoite, this age is the time of charoite crystallization. Frankamenite with an older age (137.55 ± 0.46 Ma) may reflect the polychronous crystallization of the charoite association.
作者简介
A. Ivanov
Institute of the Earth’s Crust, Siberian Branch
编辑信件的主要联系方式.
Email: aivanov@crust.irk.ru
俄罗斯联邦, Irkutsk, 664033
V. Gorovoy
Institute of the Earth’s Crust, Siberian Branch
Email: aivanov@crust.irk.ru
俄罗斯联邦, Irkutsk, 664033
D. Gladkochub
Institute of the Earth’s Crust, Siberian Branch
Email: aivanov@crust.irk.ru
俄罗斯联邦, Irkutsk, 664033
A. Shevelev
Institute of the Earth’s Crust, Siberian Branch
Email: aivanov@crust.irk.ru
俄罗斯联邦, Irkutsk, 664033
N. Vladykin
Vinogradov Institute of Geochemistry, Siberian Branch
Email: aivanov@crust.irk.ru
俄罗斯联邦, Irkutsk, 650033
补充文件
