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    Volume 36 Issue 4
    Jul.  2011
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    Article Navigation >  Earth Science  > 2011  >  36(4): 703-720
    ZHONG Yu-fang, MA Chang-qian, SHE Zhen-bing, XU Hai-jin, WANG Shi-ming, WANG Lian-xun, 2011. U-Pb-Hf Isotope of Zircons, Geochemistry and Genesis of Mengshan Granitoids in Northwestern Jiangxi Province. Earth Science, 36(4): 703-720. doi: 10.3799/dqkx.2011.071
    Citation: ZHONG Yu-fang, MA Chang-qian, SHE Zhen-bing, XU Hai-jin, WANG Shi-ming, WANG Lian-xun, 2011. U-Pb-Hf Isotope of Zircons, Geochemistry and Genesis of Mengshan Granitoids in Northwestern Jiangxi Province. Earth Science, 36(4): 703-720. doi: 10.3799/dqkx.2011.071
    shu

    U-Pb-Hf Isotope of Zircons, Geochemistry and Genesis of Mengshan Granitoids in Northwestern Jiangxi Province

    doi: 10.3799/dqkx.2011.071
    • 1.

      Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • 2.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

    • Received Date: 2010-10-08
    • Publish Date: 2011-07-01
      Abstract
    • The petrogenesis and tectonic setting of the Indosinian granites within the South China Block (SCB) are controversial, and there is no sound geochronological proof on occurrence of Indosinian magmatism in northwestern Jiangxi Province. Mengshan granitoids in this region were thought to be a Yanshanian intrusion. However, our new geochronological results show that Mengshan granites consist of three Indosinian magmatisms, with ages of 236±3 Ma, 220±3 Ma and 217±1 Ma respectively. Researches on geochemistry and Hf isotope of zircons are carried out. The Mengshan granites are metaluminous-peraluminous, having high SiO2 and K2O, with K2O+Na2O 7.53%-8.86%. The granites have ∑REE of 213.09-380.75 μg/g and REE patterns of LREE-enrichment with moderate negative Eu anomalies (Eu/Eu* = 0.07-0.40).There is strong enrichment in LILE, but showing pronounced negative anomalies in HFSE (Nb, Ta and TiO2) relative to neighbouring elements. Calculated εNd (t) values for most of samples are -9.9 to -6.1 and corresponding two-stage Nd model ages (tDM2) are 1.5-1.8 Ga. Most of the zircons from the greyish-white coarse biotite granites which were formed firstly have εHf(t) of 1.10 to 2.65, their single-stage Hf model ages tDM1 range from 782 to 866 Ma and two-stage Hf model ages tDM2 are 1 096-1 186 Ma.The zircons from the fined-grained granites which were formed thirdly in Mengshan complex have εHf(t) values of 1.71-4.98, and Hf tDM1 of 671-832 Ma and Hf tDM2 mostly are 932-1 139 Ma.The compositions of zircon Hf isotope suggest an addition of newly mantle-derived magma during the diagenesis of Mengshan granites, which provide a direct proof for the relationship between basalts underplating and the genesises of some Indonisian granites in South China. Decoupling between Nd and Hf isotopes has been found in Mengshan granites, and it probably resulted from the involvement of Neoproterozoic island-arc crust. The regularity of genentic types and the temporal-spatial distribution of the Indosinian magmatism in SCB are summarized. On this basis, the Indosinian tectonic setting and the petrogenesis of the Indosinian granites in SCB are discussed. The northwestward subduction of Pacific was probably responsible to the Indosinian magmatisms in SCB.

       

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