Accretionary orogen and evolution of the Japanese Islands-implications from a Sr-Nd isotopic study of the phanerozoic granitoids from SW Japan

American Journal of Science

Volumn 310, Issue 10, 2010, Pages 1210-1249

  Jahn, Bor Ming ^a,b  

^a INSTITUTE OF EARTH SCIENCES   (Taiwan)

^b NATIONAL TAIWAN UNIVERSITY   (Taiwan)

Author keywords

Accretionary complex; Accretionary orogen; Arabian Nubian Shield (ANS); Central Asian Orogenic Belt (CAOB); Crustal growth; Japanese Islands; Juvenile recycled crust; Mesozoic granitoids; Nipponides; SE China; Sr Nd isotope tracer; Taiwan

Indexed keywords

ACCRETIONARY PRISM; CONTINENTAL CRUST; CRUSTAL STRUCTURE; GRANITOID; ISOTOPIC RATIO; MESOZOIC; NEODYMIUM ISOTOPE; OROGENIC BELT; OROGENY; PHANEROZOIC; STRONTIUM ISOTOPE; TECTONIC EVOLUTION;

CHINA; JAPAN; SOUTH CHINA BLOCK;

EID: 79957456302     PISSN: 00029599     EISSN: None     Source Type: Journal    
DOI: 10.2475/10.2010.02     Document Type: Article

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