2024 Vol. 51, No. 4
Article Contents

ZHANG Chao, LI Zhidan, ZHANG Feng, DUAN Ming, YU Reng'an, CHEN Junqiang, XIE Yu. 2024. Zircon U–Pb age, Hf isotopic characteristics and crustal extension of the gabbro in the Yagan Cu–Ni–Co deposit, Alxa Left Banner, Inner Mongolia[J]. Geology in China, 51(4): 1368-1386. doi: 10.12029/gc20210401001
Citation: ZHANG Chao, LI Zhidan, ZHANG Feng, DUAN Ming, YU Reng'an, CHEN Junqiang, XIE Yu. 2024. Zircon U–Pb age, Hf isotopic characteristics and crustal extension of the gabbro in the Yagan Cu–Ni–Co deposit, Alxa Left Banner, Inner Mongolia[J]. Geology in China, 51(4): 1368-1386. doi: 10.12029/gc20210401001

Zircon U–Pb age, Hf isotopic characteristics and crustal extension of the gabbro in the Yagan Cu–Ni–Co deposit, Alxa Left Banner, Inner Mongolia

    Fund Project: Supported by National Key Research and Development Program (No.2018YFC0604200) and the projects of China Geological Survey (No.DD20190119, No.DD20211191, No.DD20221871, No.DD20221686).
More Information
  • Author Bio: ZHANG Chao, male, born in 1987, master, senior engineer, engaged in mineralogical research and mineral geological survey; E–mail: 402709002@qq.com
  • Corresponding author: LI Zhidan, male, born in 1986, doctoral candidate, senior engineer, engaged in mineralogical research and mineral geological survey; E–mail: cugcug@qq.com
  • This paper is the result of mineral exploration engineering.

    Objective

    The copper–nickel–cobalt deposit in the Alxa Left Banner is a typical sulfide deposit in western Inner Mongolia, developed in the ultrabasic−medium basic magmatic rock zone. The gabbro is an ore–forming rock, and recognizing the magmatic activity, metallogenic regularity and tectonic background have become an urgent geological problem.

    Methods

    Related samples were collected to study petrography, petrogeochemistry, zircon U–Pb chronology and Hf isotope.

    Results

    Geochemical characteristics shows that the Yagan gabbro has the characteristics of high Al2O3 (15.99%–17.47%), sub−alkaline (K2O+Na2O=4.94%–5.86%), low TiO2 (0.81%–1.12%), low P2O5 (0.14%–0.21%), high MgO (3.18%–5.64%), low K2O (1.14%–2.05%), indicating of the calcium alkaline series. The total amount of rare earth (ΣREE) is 71.43×10−6–94.22×10−6, presents right–inclined distribution model, the light rare earth is relatively enriched and the heavy rare earth is depleted. The high field strength elements (Nb, P, Ta) are obviously depleted, incompatible elements (U, Sr) are enriched, suggested that the Yagan gabbro originated from the lithospheric mantle and experienced crystallization differentiation in the late magmatic stage. The zircon U–Pb weighted average age of the Yagan gabbro is (268.8±3.1) Ma, indicating the age of diagenesis belongs to Middle Permian. The εHf(t) values is −7.1–2.9 and two staged Hf model age is 1272–2177 Ma.

    Conclusions

    Regional geological data and geochemical characteristics indicate that the Yagan gabbro original magma may be confused by some crustal materials during the migration process. The formation tectonic background may be the post–collision and extension environment in the Late Paleozoic. In addition, the emplacement age of Yagan gabbro limited the collision closing time, which provides new constraints for the study of Cu–Ni–Co deposits in this region.

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