Volume 46 Issue 8
Aug.  2021
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Article Navigation >  Earth Science  > 2021  >  46(8): 2887-2902
Wang Wei, Xiong Fuhao, Ma Changqian, Chen Yue, Huang Hu, 2021. Petrogenesis of Triassic Suolagou Sanukitoid-like Diorite in East Kunlun Orogen and Its Implications for Paleo-Tethyan Orogeny. Earth Science, 46(8): 2887-2902. doi: 10.3799/dqkx.2020.270
Citation: Wang Wei, Xiong Fuhao, Ma Changqian, Chen Yue, Huang Hu, 2021. Petrogenesis of Triassic Suolagou Sanukitoid-like Diorite in East Kunlun Orogen and Its Implications for Paleo-Tethyan Orogeny. Earth Science, 46(8): 2887-2902. doi: 10.3799/dqkx.2020.270
shu

Petrogenesis of Triassic Suolagou Sanukitoid-like Diorite in East Kunlun Orogen and Its Implications for Paleo-Tethyan Orogeny

doi: 10.3799/dqkx.2020.270
  • 1.

    College of Earth Science, Chengdu University of Technology, Chengdu 610059, China

  • 2.

    State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China

  • 3.

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

  • Received Date: 2020-08-16
    Available Online: 2021-09-14
  • Publish Date: 2021-08-15
    Abstract
  • Sanukitoid with special genetic mechanism is one important petrological probe to study the magma dynamic processes and associated tectonic process. In this study, it presents petrology, geochronology, elemental geochemistry and Lu-Hf isotopic data on the Suolagou sanukitoid-like diorite in East Kunlun, aiming to characterize its petrogenesis and to reveal its implications on the Paleo-Tethyan orogeny. Zircon U-Pb dating shows that the Suolagou diorite was formed in the Middle Triassic (~243 Ma). Geochemically, they have low contents of SiO2(50.26%-57.40%), but high contents of total alkaline (Na2O+K2O=3.5%-6.3%), MgO (6.0%-7.1%) and high Mg# (50.1-60.9), belonging to high magnesium, calc-alkaline and metaluminous series. The Suolagou diorites show geochemical similarities to high Mg# andesitic sanukitoids with high contents of Sr (622×10-6-1 041×10-6), Cr (30×10-6-161×10-6) and Ni (19×10-6-79×10-6), and moderate contents of Y(7.6×10-6-24.3×10-6) and Yb(0.62×10-6-1.87×10-6). These rocks display remarkable enrichment in light rare earth elements and large-ion lithophile elements (such as Cs, Rb, K and Pb) but depletion in high-field strength elements (such as Ta, Nb and Zr), resembling the arc-related magmatic rocks above subduction zone. Lu-Hf isotopes show that the Suolagou diorites were derived from partial melting of enriched lithospheric mantle (εHf(t)=-2.4 to -0.4, TDM=0.89-0.99 Ga). The~243 Ma sanukitoid-like diorite in East Kunlun were formed in a continental arc setting, i.e., the parent magma derived from partial melting of enriched lithospheric mantle, subsequently followed by fractional crystallization of amphibole and biotite. This study suggests that the transition from Paleo-Tethyan oceanic slab subduction to terranes collision in East Kunlun occurred at Middle Triassic, and the Suolagou sanukitoid-like high-Mg diorites could be the magmatic response to the slab break-off at the end of subduction.

     

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