Neoproterozoic (∼ 800 Ma) orogeny in the Tuva-Mongolia Massif (Siberia): Island arc-continent collision at the northeast Rodinia margin

Precambrian Research

Volumn 110, Issue 1-4, 2001, Pages 109-126

  Kuzmichev, A B ^a   Bibikova, E V ^b   Zhuravlev, D Z ^c  

^a Institute of the Lithosphere of Marginal Seas   (Russian Federation)

^b VERNADSKY INSTITUTE OF GEOCHEMISTRY AND ANALYTICAL CHEMISTRY   (Russian Federation)

^c INSTITUTE OF GEOLOGY OF ORE DEPOSITS   (Russian Federation)

Author keywords

Forearc ophiolite; Island arc continent collision; Neoproterozoic; Rodinia; Siberia; Tonalite; Tuva Mongolia Massif

Indexed keywords

LEAD; URANIUM; ZIRCONIUM;

ARC-CONTINENT COLLISION; OROGENIC BELT; PROTEROZOIC; RODINIA;

CHRONOLOGY; EVOLUTION; GEOGRAPHY; GEOLOGY; MONGOLIA; REVIEW; RUSSIAN FEDERATION; VOLCANO;

RUSSIAN FEDERATION;

EID: 0035420665     PISSN: 03019268     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0301-9268(01)00183-8     Document Type: Article

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