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)

Russian Geology and Geophysics

Volumn 52, Issue 5, 2011, Pages 503-516

  Mongush, A A ^a   Lebedev, V I ^a   Kovach, V P ^b   Sal'nikova, E B ^b   Druzhkova, E K ^a   Yakovleva, S Z ^b   Plotkina, Yu V ^b   Zagornaya, N Yu ^b   Travin, A V ^c   Serov, P A ^d  

^a Tuva Institute for Exploration of Natural Resources of the Siberian Branch of the RAS   (Russian Federation)

^b INSTITUTE OF PRECAMBRIAN GEOLOGY AND GEOCHRONOLOGY   (Russian Federation)

^c SOBOLEV INSTITUTE OF GEOLOGY AND MINERALOGY   (Russian Federation)

^d GEOLOGICAL INSTITUTE   (Russian Federation)

Author keywords

Accretion; Cambrian; Geodynamics; Island arc; Subduction; Tuva; Vendian

Indexed keywords

ACCRETIONARY PRISM; ACTIVE MARGIN; CAMBRIAN; CONTINENTAL MARGIN; FOLD BELT; GEOCHEMISTRY; GEOCHRONOLOGY; GEODYNAMICS; ISLAND ARC; MAGMATISM; MANTLE SOURCE; NEODYMIUM ISOTOPE; SUBDUCTION; TECTONIC EVOLUTION; VENDIAN;

RUSSIAN FEDERATION; TUVA;

EID: 79955041477     PISSN: 10687971     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.rgg.2011.04.003     Document Type: Article

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