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)


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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.

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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