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    Petrogenesis and tectonic setting of Triassic granitoids in the Qiangtang terrane, central Tibet: Evidence from U-Pb ages, petrochemistry and Sr-Nd-Hf isotopes

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    Fulltext not available
    Authors
    Li, G.
    Li, J.
    Zhao, J.
    Qin, K.
    Cao, M.
    Evans, Noreen
    Date
    2014
    Type
    Journal Article
    
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    Citation
    Li, G. and Li, J. and Zhao, J. and Qin, K. and Cao, M. and Evans, N. 2014. Petrogenesis and tectonic setting of Triassic granitoids in the Qiangtang terrane, central Tibet: Evidence from U-Pb ages, petrochemistry and Sr-Nd-Hf isotopes. Journal of Asian Earth Sciences.
    Source Title
    Journal of Asian Earth Sciences
    DOI
    10.1016/j.jseaes.2015.02.017
    ISSN
    1367-9120
    School
    Department of Applied Geology
    URI
    http://hdl.handle.net/20.500.11937/41868
    Collection
    • Curtin Research Publications
    Abstract

    Triassic granitoids, including the ~220Ma Shuanghu and ~210Ma Rongma granitoids studied here, are widely distributed around the Longmu-Shuanghu suture and in the Qiangtang terrane, central Tibet. The majority of these granitoids can be classified as high-K calc-alkaline in nature and yield negative Ba and Sr anomalies on primitive mantle-normalized diagrams. In addition, they are: enriched in light rare earth elements (LREE) ((La/Yb)N =1.61-21.79); strongly enriched in large ion lithophile elements (LILE: e.g., Cs, Rb, and K), and depleted in high field strength elements (HFSE: e.g., Nb and Ti). Magma mixing played a role in the genesis of the Shuanghu granodiorites, as indicated by the occurrence of dioritic enclaves and the wide range in zircon Hf compositions (eHf(t)=-15.0 to -2.5). The I-type Shuanghu granodiorites and S-type Shuanghu and Rongma granites might have been derived from melting of southern Qiangtang crust given the high initial Sr (0.7131-0.7272), low eNd(t) (-8.9 to -11.1) and zircon eHf(t) values (-15 to -7.2). The granitoids may have formed during melting of southern Qiangtang crust, heated by upwelling asthenosphere mantle, a result of break-off and delamination of the Paleo-Tethys slab in a collisional setting.

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