Volume 43 Issue 12
Dec.  2018
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Li Ruibao, Pei Xianzhi, Li Zuochen, Pei Lei, Chen Guochao, Li Xiaobing, Chen Youxin, Liu Chengjun, Wei Bo, 2018. Geochemistry and Tectonic Setting of Qingquangou Forearc Basalts in Central Tectonic Mélange of East Kunlun Orogen. Earth Science, 43(12): 4521-4535. doi: 10.3799/dqkx.2018.540
Citation: Li Ruibao, Pei Xianzhi, Li Zuochen, Pei Lei, Chen Guochao, Li Xiaobing, Chen Youxin, Liu Chengjun, Wei Bo, 2018. Geochemistry and Tectonic Setting of Qingquangou Forearc Basalts in Central Tectonic Mélange of East Kunlun Orogen. Earth Science, 43(12): 4521-4535. doi: 10.3799/dqkx.2018.540
shu

Geochemistry and Tectonic Setting of Qingquangou Forearc Basalts in Central Tectonic Mélange of East Kunlun Orogen

doi: 10.3799/dqkx.2018.540
  • 1.

    School of Earth Science and Resources, Chang'an University, Xi'an 710054, China

  • 2.

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

  • Received Date: 2018-02-10
  • Publish Date: 2018-12-15
    Abstract
  • The research on magmatic source and tectonic setting of Qingquangou basalts in eastern section of East Kunlun is important for discussion of the tectonic evolution of East Kunlun ocean. This paper presents a systematic field geology, geochemistry, and tectonic setting research. The results show that the SiO2 contents of Qingquangou basalts range from 48.60% to 49.28%, MgO contents range from 7.72%-8.00%, TiO2 contents range from 1.07%-1.10% (average values, 1.09%), which are similar to the values of Izu-Bonin-Mariana forearc basalt, West Pacific. The basalts are classified into the tholeiitic basalt of subalkaline series based on the major elements feature. Qingquangou basalts are characterized by the ∑LREEs range from 22.64×10-6-33.31×10-6, ∑HREEs range from 13.13×10-6-18.37×10-6, ∑REEs range from 36.02×10-6-51.68×10-6, and (La/Yb)N range from 0.88-1.10. The chondrite normalized REE patterns show the widely enriched-depleted feature of LREE, resembling the feature of NMORB basalts and IBM forearc basalts, West Pacific. Moreover, the samples have low ratios of Ti/Y (312) and Ti/V (< 20), also indicative of the forearc basalt feature. The primitive mantle normalized trace element spider diagram shows enriched LILEs and undifferentiated HFSEs (e.g., Nb, Ta, Zr, Hf, etc.) features. Petrogenesis research shows that its source was derived from the depleted mantle, and further proves that its partial melting degree is higher than that of NMORB-type basalts. Additionally, the tectonic discrimination diagram suggests that the basalts formed in forearc tectonic setting. Combined with the previous data, it is concluded that East Kunlun ocean began to subduct northward at Middle Cambrian (ca.510 Ma), and that Qingquangou forearc basalts were generated meanwhile, forming the nascent island arc crust.

     

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