Abstract: 886-857 Ma granites from Yenisey Ridge formed long before their collision with the western margin of the Siberian Craton (2015 AGU Fall Meeting)

886-857 Ma granites from Yenisey Ridge formed long before their collision with the western margin of the Siberian Craton

Valery Vernikovsky¹, Antonina E. Vernikovskaya^1,2, Dmitry V. Metelkin^1,3, Aleksey Y. Kazansky⁴, Nikolay Yu Matushkin³, Pavel I. Kadilnikov^1,3, Irina Romanova³, Alexandr N. Larionov⁵ and Michael T D Wingate⁶, (1)Novosibirsk State University, Novosibirsk, Russia, (2)Novosibirsk State University, Trofimuk Institute of Petroleum Geology and Geophysics SB RAS, Geology and Geophysics, Novosibirsk, Russia, (3)Trofimuk Institute of Petroleum Geology and Geophysics SB RAS, Novosibirsk, Russia, (4)Moscow State University, Moscow, Russia, (5)A.P.Karpinsky Russian Geological Research Institute, S.Petersburg, Russia, (6)Geological Servey of Western Australia, Perth, Australia

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