Phanerozoic evolution of the Inner Mongolia-Daxinganling orogenic belt in North China: Constraints from geochronology of ophiolites and associated formations

Geological Society Special Publication

Volumn 280, Issue , 2007, Pages 223-237

  Miao, L ^a   Zhang, F ^a   Fan, W M ^a   Liu, D ^b  

^a INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

^b INSTITUTE OF GEOLOGY   (China)

Author keywords

[No Author keywords available]

Indexed keywords

BASIN EVOLUTION; CONTINENTAL COLLISION; CONTINENTAL MARGIN; GEOCHRONOLOGY; GRANITOID; METAMORPHIC ROCK; OCEAN BASIN; OPHIOLITE; ORDOVICIAN; OROGENIC BELT; PHANEROZOIC; SUBDUCTION; TECTONIC EVOLUTION;

ASIA; CHINA; DA HINGGAN MOUNTAINS; EURASIA; FAR EAST; NEI MONGGOL; NORTH CHINA BLOCK; SOUTH CHINA BLOCK;

EID: 34447554583     PISSN: 03058719     EISSN: None     Source Type: Book Series    
DOI: 10.1144/SP280.11     Document Type: Article

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