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ZHU Qingbo, JIN Guodong, ZHAO Xilin, ZHANG Chuanlin, SHU Xujie, HONG Wentao. 2020. Petrogenesis of the late Mesozoic Lingshang ultramafic intrusion in northern Jiangxi Province:Chronologic and geochemical constraints[J]. Geology in China, 47(4): 1092-1108. doi: 10.12029/gc20200413
Citation: ZHU Qingbo, JIN Guodong, ZHAO Xilin, ZHANG Chuanlin, SHU Xujie, HONG Wentao. 2020. Petrogenesis of the late Mesozoic Lingshang ultramafic intrusion in northern Jiangxi Province:Chronologic and geochemical constraints[J]. Geology in China, 47(4): 1092-1108. doi: 10.12029/gc20200413
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Petrogenesis of the late Mesozoic Lingshang ultramafic intrusion in northern Jiangxi Province:Chronologic and geochemical constraints

  • 1.

    China Geological Survey Nanjing Geological Survey Center, Nanjing 210016, Jiangsu, China

  • 2.

    Hohai University, Nanjing 210016, Jiangsu, China

  • 3.

    Nanjing University, Nanjing 210023, Jiangsu, China

    • Fund Project: Supported by the project of China Geological Survey(No. DD20190045)
More Information
  • Author Bio: ZHU Qingbo, male, born in 1986, assistant researcher, majors in survey and study of Orogenic belt; Email:zhuqingbo1234@163.com
Received Date:  29 April 2019
Revised Date:  19 April 2020
Publish Date:  25 August 2020
    Abstract

  • Extensive lithospheric extensional thinning events occurred during the late Mesozoic in the interior of South China block. As a record of the early Cretaceous ((120.8±1.4)Ma) mantle-derived magmatic activities in the eastern part of the Qingzhou-Hangzhou juncture belt, the Lingshang ultramafic intrusion in Xinyu of northern Jiangxi is a good object for studying the mantle attribute and geodynamic process of the late Mesozoic in central South China. Based on a systematic analysis of the geochronology from La-MC-ICP-MS zircon U-Pb, Lu -hf isotopes and element geochemistry of the Lingshang ultramafic rocks, the authors investigated the intrusion, the source area characteristics of the ultramafic intrusion and the tectonic background reflected by them. Lingshang ultramafic intrusion suffered no significant crustal contamination. The content of MgO is concentrated with no obvious linear relationship with TiO2, Al2O3, Ni, Th, and some other components, implying no significant crystallization differentiation. However, the range of Mg# and La-Sm differentiation indicates that heap crystallization and partial melting might have exerted an effect on magmatic evolution. The characteristics of rare earth and trace elements (Nb, Ta, Zr, Hf, etc.) are similar to those of intraplate basalt (OIB), and the characteristics of low SiO2, high Ti, high Fe/Mn ratio and Ni are all closely related to asthenosphere mantle. However, the εHf(t) of zircons (6.83-11.41) are less than the value of the depleted mantle, and Nb/Ta ratios are close to the ratio of lithospheric mantle, suggesting low degree partial melting of spinel peridotite mantle source region in the relevant element diagram. All of these data suggest that the Lingshang ultramafic intrusion may be the result of the interaction between asthenosphere mantle and lithospheric mantle under the background of late Mesozoic intracontinental extension. The upwelling asthenosphere material led to the low-degree partial melting of the preexisting spinel peridotite mantle source area, and the deep ultramafic magma was emplaced rapidly along the tectonic weak zone to form the Lingshang ultramafic intrusion.

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