Monday, 14 December 2015
Poster Hall (Moscone South)
Dmitry V. Metelkin1,2, Valeriy A. Vernikovskiy1,2, Nikolay Yu Matushkin1,2, Anna Zhdanova1,2, Nikolay E Mikhaltsov1,2, Viktor V Abashev1,2 and Evgeniy Kulakov1,2, (1)Novosibirsk State University, Novosibirsk, Russia, (2)Trofimuk Institute of Petroleum Geology and Geophysics SB RAS, Novosibirsk, Russia

We report paleomagnetic and geologic data that support a new plate tectonic reconstruction for the Arctic from the Neoproterozoic to Mesozoic. We propose a new outlook on the history of the Arctida paleocontinent, which combined sialic blocks of the present Eurasian shelf of the Arctic Ocean. Our model implies two Arctidas at that time. The earlier Arctida-I was located near equator and connected the continental margins of Laurentia, Baltica and Siberia within the supercontinent of Rodinia. The Arcrtida-I disintegration was caused by a breakup of Rodinia. As a result, small plates like on Svalbard, Kara, New Siberia Island (NSI) terrane and others were formed. We have reconstructed the main stages of later remobilization and global drift of these plates before Pangea assemblage. In contrast to traditional interpretation of the NSI as a part of the Chukchi-Alaska terrane, our observation suggest a linkage between the NSI and Kolyma-Omolon terrane that framed Siberia. As a result of Pangea assembly at Paleozoic-Mesozoic boundary the second recovery of Arctida took place. We assume that Arctida-II also connected Laurentia, Baltica, and Siberia but constituted the Pangean periphery in the temperate latitudes. The later Arctida-II disintegrated during the Mesozoic during the opening of Arctic Ocean.