The Early Paleozoic Active Margin of the Khangai Segment of the Mongol–Okhotsk Ocean

Pleiades Publishing Ltd - Tập 480 Số 1 - Trang 559-563 - 2018
V. V. Yarmolyuk1, И. К. Козаков2, A. M. Kozlovsky3, E. A. Kudryashova3, А. В. Травин4,5,6, T. I. Kirnozova7, M. M. Fugzan7, Yu. V. Plotkina2
1
2Institute of Precambrian Geology and Geochronology, Russian Academy of Sciences, St. Petersburg, Russia
3Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences, Moscow, Russia
4Novosibirsk State University, Novosibirsk, Russia
5Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia
6Tomsk State University, Tomsk, Russia
7Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, Moscow, Russia

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