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The tectonomagmatic evolution of structure-lithologic complexes in the Tannu-Ola zone, Tuva, in the Late Vendian–Early Cambrian (from geochemical, Nd isotope, and geochronological data)
Authors:AA Mongush  VI Lebedev  VP Kovach  EB Sal&#x;nikova  EK Druzhkova  SZ Yakovleva  YuV Plotkina  NYu Zagornaya  AV Travin  PA Serov
Institution:a Tuvinian Institute of Complex Exploration of Natural Resources, Siberian Branch of the Russian Academy of Sciences, ul. Internatsional’naya 117a, Kyzyl, 667007, Russia;b Institute of the Precambrian Geology and Geochronology, nab. Makarova 2, St. Petersburg, 199034, Russia;c V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia;d Geological Institute of the Kola Research Center, Russian Academy of Sciences, ul. Fersmana 14, Apatity, Murmansk Region, 184209, Russia
Abstract:
Keywords:island arc  subduction  accretion  geodynamics  Vendian  Cambrian  Tuva
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