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    Volume 44 Issue 7
    Jul.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(7): 2461-2477
    Zhang Yongming, Pei Xianzhi, Li Zuochen, Li Ruibao, Liu Chengjun, Pei Lei, Chen Youxin, Wang Meng, 2019. Zircon U-Pb Geochronogy, Geochemistry and Its Geological Implication of the Early Indosinian Basic Complex in the Qinghai Nanshan Tectonic Belt. Earth Science, 44(7): 2461-2477. doi: 10.3799/dqkx.2018.537
    Citation: Zhang Yongming, Pei Xianzhi, Li Zuochen, Li Ruibao, Liu Chengjun, Pei Lei, Chen Youxin, Wang Meng, 2019. Zircon U-Pb Geochronogy, Geochemistry and Its Geological Implication of the Early Indosinian Basic Complex in the Qinghai Nanshan Tectonic Belt. Earth Science, 44(7): 2461-2477. doi: 10.3799/dqkx.2018.537
    shu

    Zircon U-Pb Geochronogy, Geochemistry and Its Geological Implication of the Early Indosinian Basic Complex in the Qinghai Nanshan Tectonic Belt

    doi: 10.3799/dqkx.2018.537
    • 1.

      Key Laboratory of Western China's Mineral Resources and Geological Engineering, Ministry of Education, Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, School of Earth Science and Resources, Chang'an University, Xi'an, 710054, China

    • 2.

      Faculty of Resources and Environmental Engineering, Shandong University of Technology, Zibo 255049, China

    • Received Date: 2018-02-09
    • Publish Date: 2019-07-15
      Abstract
    • The Qinghai Nanshan tectonic belt, situated in the northern margin of Gonghe basin, is the conjunction area among the West Qinling orogenic belt, South Qilian tectonic belt and Zongwulong tectonic belt. A large quantity of intrusive rocks outcropped in the Qinghai Nanshan tectonic belt, but the distribution of basic rocks is less and dispersed. The petrogenesis of basic rocks is significant to reveal the tectonic framework and evolution history in that period.The Lari basic complex is composed of gabbro and pyroxenite, which situates in the middle of the Qinghai Nanshan tectonic belt. In this paper, a detailed study on petrology, mineralogy, geochemistry and LA-ICP-MS zircon U-Pb dating was carried out for the Lari basic complex. The results show that the crystallization ages of the gabbro and pyroxenite are 247.7±2.8 Ma and 247.9±2.5 Ma, respectively, suggesting that the complex intruded in the late Early Triassic. The whole rock geochemical data show that the rocks of Lari basic complex are relatively rich in Na, Mg and Fe, but poor in Si and K, suggesting that the gabbros belong to the tholeiitic series. What's more, they have high ratios of Al2O3/TiO2, low contents of TiO2, which are typical features of boninite and boni-basalts. The rocks are enriched in LREE, LILEs (Cs, Rb, K, Sr) and depleted in HREE (Nb, Ta, Zr, Hf, Ti, P), which are similar to the arc magma, but different from ridge and intraplate basalt. The mineral electron microprobe analysis shows that plagioclase in the rocks of Lari basic complax is similar to the high calcium plagioclase in gabbro which originates in the island arc or active continental margin. The gabbro and pyroxenite of the Lari basic complex were formed by partial melting of the spinel lherzolite. In combination with analyses of regional geological setting, we suggest that there existed a Late Paleozoic-Early Mesozoic limited oceanic basin in the Qinghai Nanshan area. The Lari basic complex formed during the early stage of the oceanic basin subduction.

       

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