Hafnium–Neodymium Isotope Systematics of Carbonatites from the Guli Massif (Maimecha–Kotui Province, Russia)
- 作者: Malitch K.1, Kogarko L.2, Badanina I.1, Belousova E.3
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隶属关系:
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch
- Vernadsky Institute of Geochemistry and Analytical Chemistry
- Macquarie University
- 期: 卷 480, 编号 1 (2018)
- 页面: 652-655
- 栏目: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/193176
- DOI: https://doi.org/10.1134/S1028334X18050240
- ID: 193176
如何引用文章
详细
This work presents new data on the Hf-isotope systematics of baddeleyite and the Nd-isotope compositions of calcite carbonatites of the Guli massif, located within the Maimecha–Kotui province. The Hf–Nd isotope signatures of carbonatites (εHf ~ 10.4, εNd ~ 5.8) indicate that depleted mantle material was involved during magma generation. The application of the Hf–Nd isotope systematics provided an essential tracer for the depleted mantle contribution into the source of carbonatites from the Guli Massif.
作者简介
K. Malitch
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
编辑信件的主要联系方式.
Email: dunite@yandex.ru
俄罗斯联邦, Yekaterinburg, 620016
L. Kogarko
Vernadsky Institute of Geochemistry and Analytical Chemistry
Email: dunite@yandex.ru
俄罗斯联邦, Moscow, 199119
I. Badanina
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: dunite@yandex.ru
俄罗斯联邦, Yekaterinburg, 620016
E. Belousova
Macquarie University
Email: dunite@yandex.ru
澳大利亚, Sydney, NSW, 2109