The U–Pb System in Schorlomite from Calcite–Amphobole–Pyroxene Pegmatite of the Afrikanda Complex (Kola Peninsula)
- 作者: Salnikova E.B.1, Stifeeva M.V.1, Chakhmouradian A.R.2, Glebovitsky V.A.1, Reguir E.P.2
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隶属关系:
- Institute of Precambrian Geology and Geochronology
- University of Manitoba
- 期: 卷 478, 编号 2 (2018)
- 页面: 148-151
- 栏目: Geology
- URL: https://ogarev-online.ru/1028-334X/article/view/192117
- DOI: https://doi.org/10.1134/S1028334X18020083
- ID: 192117
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详细
The geochronological U–Pb study of shorlomite from igneous rocks of the alkali–ultramafic Afrikanda massif (Kola Peninsula) was performed. The results demonstrate the reliability of calcium garnet as a mineral for the U–Pb geochronology of a wide range of igneous rocks, i.e., carbonatite, syenite, foidolite, foidite, melilitolite, melilitite, lamprophyres, micaceous kimberlites, etc., and associated rare earth and trace elements (REE, Nb, Zr) mineralization.
作者简介
E. Salnikova
Institute of Precambrian Geology and Geochronology
编辑信件的主要联系方式.
Email: katesalnikova@yandex.ru
俄罗斯联邦, St. Petersburg, 199034
M. Stifeeva
Institute of Precambrian Geology and Geochronology
Email: katesalnikova@yandex.ru
俄罗斯联邦, St. Petersburg, 199034
A. Chakhmouradian
University of Manitoba
Email: katesalnikova@yandex.ru
加拿大, Winnipeg
V. Glebovitsky
Institute of Precambrian Geology and Geochronology
Email: katesalnikova@yandex.ru
俄罗斯联邦, St. Petersburg, 199034
E. Reguir
University of Manitoba
Email: katesalnikova@yandex.ru
加拿大, Winnipeg
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