The geodynamic evolution of the folded framing and the western margin of the Siberian craton in the Neoproterozoic: geological, structural, sedimentological, geochronological, and paleomagnetic data

Russian Geology and Geophysics

Volumn 50, Issue 4, 2009, Pages 380-393

  Vernikovsky, V A ^a,b   Kazansky, A Yu ^a,b   Matushkin, N Yu ^a,b   Metelkin, D V ^a,b   Sovetov, J K ^a,b  

^a TROFIMUK INSTITUTE OF PETROLEUM GEOLOGY AND GEOPHYSICS   (Russian Federation)

^b NOVOSIBIRSK STATE UNIVERSITY   (Russian Federation)

Author keywords

geodynamics; kinematics; Neoproterozoic igneous complexes; paleomagnetism; rift and foreland sedimentary basins; Siberian craton; Yenisei fault zone; Yenisei Ridge

Indexed keywords

CONTINENTAL MARGIN; CRATON; FAULT ZONE; FOLD AND THRUST BELT; FORELAND BASIN; GEOCHRONOLOGY; GEODYNAMICS; ISLAND ARC; KINEMATICS; OPHIOLITE; OROGENY; PALEOMAGNETISM; PASSIVE MARGIN; PROTEROZOIC; RIFTING;

EURASIA; RUSSIAN FEDERATION; SIBERIAN PLATFORM;

EID: 62849087254     PISSN: 10687971     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.rgg.2009.03.014     Document Type: Article

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