Correlation of High-Calcium Silica-Undersaturated Complex of the Maymecha–Kotuy Province with Siberian Flood Basalts: New Age Data on the Kugda Massif (Polar Siberia)
- Authors: Anosova M.O.1, Kostitsyn Y.A.1, Kogarko L.N.1
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Affiliations:
- Vernadsky Institute of Geochemistry and Analytical Chemistry
- Issue: Vol 57, No 12 (2019)
- Pages: 1339-1342
- Section: Short Communications
- URL: https://journals.rcsi.science/0016-7029/article/view/156400
- DOI: https://doi.org/10.1134/S0016702919120048
- ID: 156400
Cite item
Abstract
Abstract—Perovskite crystals from the ore-bearing olivinite and phoscorite of the Kugda massif were analyzed by LA-ICP-MS. Age obtained for the alkaline rocks of the Kugda massif is 257 ± 6 Ma. This implies that the Kugda massif was formed simultaneously with the Siberian flood basalts and Guli Massif (250 ± 9 Ma), which is the largest and highly differentiated pluton in the Maymecha–Kotuy Province. The simultaneous formation of the melilite-bearing Kugda Complex, Siberian flood basalts, and Guli Massif suggests the possible genetic relation of these rocks.
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About the authors
M. O. Anosova
Vernadsky Institute of Geochemistry and Analytical Chemistry
Author for correspondence.
Email: anosova@geokhi.ru
Russian Federation, ul. Kosygina, 19, Moscow, 119991
Yu. A. Kostitsyn
Vernadsky Institute of Geochemistry and Analytical Chemistry
Author for correspondence.
Email: kostitsyn@geokhi.ru
Russian Federation, ul. Kosygina, 19, Moscow, 119991
L. N. Kogarko
Vernadsky Institute of Geochemistry and Analytical Chemistry
Author for correspondence.
Email: kogarko@geokhi.ru
Russian Federation, ul. Kosygina, 19, Moscow, 119991
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