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SHE Jianzhong, CHEN Gang, ZHU Zhixin, JIA Jian, DI Xiaochen, DONG Guosheng, LIU Kaixuan, JIN Cheng. 2021. Geochemistry, zircon chronology, Sr-Nd-Hf isotopic characteristics and subduction magmatism of Heishidun basic rocks in the East Tianshan[J]. Geology in China, 48(4): 1239-1254. doi: 10.12029/gc20210419
Citation: SHE Jianzhong, CHEN Gang, ZHU Zhixin, JIA Jian, DI Xiaochen, DONG Guosheng, LIU Kaixuan, JIN Cheng. 2021. Geochemistry, zircon chronology, Sr-Nd-Hf isotopic characteristics and subduction magmatism of Heishidun basic rocks in the East Tianshan[J]. Geology in China, 48(4): 1239-1254. doi: 10.12029/gc20210419
shu

Geochemistry, zircon chronology, Sr-Nd-Hf isotopic characteristics and subduction magmatism of Heishidun basic rocks in the East Tianshan

  • 1.

    Xinjiang Uygur Autonomous Region Geology Survey Institute, Urumqi 830000, Xinjiang, China

  • 2.

    Scholl of Geology and Exploration Engineering, Xinjiang University, Urumqi 830046, Xinjiang, China

  • 3.

    College of Geosciences, China University of Geosciences, Wuhan 430000, Hubei, China

    • Fund Project: Supported by the project of China Geological Survey (No. 12120114059201)
More Information
  • Author Bio: SHE Jianzhong, male, born in 1982, master, senior engineer, engaged in regional geology and mineral investigation; E-mail: sjz832@163.com
Received Date:  03 April 2019
Revised Date:  06 May 2020
Publish Date:  25 August 2021
    Abstract

  • A new set of basic rocks was discovered in the Heishidun in South Kangurtag, Eastern Tianshan. Its lithology mainly consists of gabbro and olive gabbro. The rocks are characterized by relatively low contents of SiO2 (47.59%-50.79%), K2O (0.26%-1.15%) and MgO (3.94%-12.55%), high contents of Na2O (2.72% -4.42%) and Al2O3 (14.75% -19.65%), and moderate content of Mg# (47.6-66.64). Light rare earth is enriched ((La/Yb)N of 1.83-2.12) with a bit of Eu positive anomaly (1.00-1.25). LILE (Ba, U, Sr) is enriched, while HFS (Ta, Nb, Th, and Ti) is depleted, and Pb is strongly enriched. LA-ICP-MS zircon U-Pb dating yields 342.6±3.2 Ma, indicating that this basic rock is a product of Early Carboniferous magmatic activity. Rocks have lower Sr ratio (87Sr/86Sr)i (0.703421-0.704551), positive εNd (t) (7.6-8.1) and εHf (t) (9.82-13.74). Geochemical characteristics and petrography show that it is originated from the lithospheric mantle source of the loss, and the source area was affected by the metamorphism of the dehydration and melting fluids resulted from the subduction of marine sediments rich in large ionic lithophile and light rare earth elements. The separation and crystallization of olivine, pyroxene and plagioclase took place during the emplacement of magma, the degree of contamination by the crustal material during the emplacement was very low. The structural and dynamic background shows that the Heishidun basic rock is the product of the Northern Tianshan Ocean's northward subduction along the Kangugtag-Huangshan fault in the Early Carboniferous.

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