Zircon ages and Hf isotopic constraints on sources of clastic metasediments of the Slyudyansky high-grade complex, southeastern Siberia: Implication for continental growth and evolution of the Central Asian Orogenic Belt

Journal of Asian Earth Sciences

Volumn 62, Issue , 2013, Pages 18-36

  Kovach, Victor ^a   Salnikova, Ekaterina ^a   Wang, Kuo Lung ^b   Jahn, Bor Ming ^b,c   Chiu, Han Yi ^c   Reznitskiy, Leonid ^d   Kotov, Alexander ^a   Iizuka, Yoshiyuki ^b   Chung, Sun Lin ^c  

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

^b INSTITUTE OF EARTH SCIENCES   (Taiwan)

^c NATIONAL TAIWAN UNIVERSITY   (Taiwan)

^d INSTITUTE OF THE EARTH S CRUST   (Russian Federation)

Author keywords

Central Asian Orogenic Belt; Continental growth; Nd Hf isotopes; Slyudyansky Complex; Zircon ages

Indexed keywords

AGE DETERMINATION; CLASTIC SEDIMENT; CONTINENTAL CRUST; CRUSTAL EVOLUTION; CRYSTALLIZATION; DEPOSITION; ISOTOPIC COMPOSITION; METASEDIMENT; NEODYMIUM ISOTOPE; OROGENIC BELT; PALEOZOIC; PROTEROZOIC; PROVENANCE; TERRANE; URANIUM-LEAD DATING;

CENTRAL ASIA; LAKE BAIKAL; RUSSIAN FEDERATION; SIBERIA;

EID: 84872801912     PISSN: 13679120     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.jseaes.2011.08.008     Document Type: Article

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