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LI Yan, CHENG Chun, SU Shaoming, GAO Jianfeng, HUANG Feixin, XIONG Yingzhi, ZHANG Yan, HUANG Hua. Sr-Nd and zircon Hf isotopic constraints on petrogenesis of the Early Cretaceous diorite in the Jinjingzui gold deposit, southeast Hubei Province[J]. GEOLOGY IN CHINA, 2023, 50(5): 1573-1585. DOI: 10.12029/gc20200611002
Citation: LI Yan, CHENG Chun, SU Shaoming, GAO Jianfeng, HUANG Feixin, XIONG Yingzhi, ZHANG Yan, HUANG Hua. Sr-Nd and zircon Hf isotopic constraints on petrogenesis of the Early Cretaceous diorite in the Jinjingzui gold deposit, southeast Hubei Province[J]. GEOLOGY IN CHINA, 2023, 50(5): 1573-1585. DOI: 10.12029/gc20200611002

Sr-Nd and zircon Hf isotopic constraints on petrogenesis of the Early Cretaceous diorite in the Jinjingzui gold deposit, southeast Hubei Province

Funds: 

the National Key R&D Program of China 2016YFC0600207

Science Foundation of Institute of Mineral Resources Research, China Metallurgical Geology Bureau 

More Information
  • Author Bio:

    LI Yan, male, born in 1988, senior engineer, mainly engaged in petrology and metallogeny survey; E-mail: liyan@cmgb.cn

  • Corresponding author:

    CHENG Chun, born in 1969, professor of engineering, mainly engaged in metallogeny survey; E-mail: chengchun@cmgb.cn

  • Received Date: June 10, 2020
  • Revised Date: August 24, 2020
  • Available Online: November 17, 2023
  • This paper is the result of geological survey engineering.

    Objective 

    The petrogenesis and magmatic origin of the early Cretaceous diorite in Jinjingzui gold deposit are of great significance for the diagenetic and metallogenic relations and perfecting the regional metallogenic regularity.

    Methods 

    In this study we report the Sr-Nd and zircon Hf isotopic compositions of diorite in Jinjingzui deposit.

    Results 

    The results show that the diorite has relative high initial 87Sr/86Sr ratio (0.7059-0.7062), negative εNd(t) values (-7.93--7.58) and εHf(t) values (-12.2--6.5), suggesting the magma was derived from partial melting of an enrichment mantle, followed by magma differentiation. There may be continental crust contamination during magmatic evolution.

    Conclusions 

    By comparison with reported deposit in cluster, Jinjingzui Au deposit is similar to these Au deposit at Edong cluster in rock- and ore-forming ages, petrogenesis and magma source. However, the gold orebody of Jinjingzui Au deposit mainly lay within the diorite body, which is obviously different from other deposits that lay internal or external contact zone of rocks. The discovery of Jinjingzui deposit is of great significance for perfecting regional metallogenic regularity and gold prospecting and exploration.

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