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    Volume 49 Issue 3
    Mar.  2024
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    Article Navigation >  Earth Science  > 2024  >  49(3): 803-821
    Qin Ya, Yang Junru, Feng Zuohai, Zhu Jiaming, Ni Zhanxu, Huang Yonggao, Wu Jie, Zhou Yun, Liu Yizhi, Bai Yuming, 2024. Mineralogy and Mineral Chemistry of the Luojiashan Gabbro in the Yingyangguan Area of Northeastern Guangxi and Its Tectonic Significance. Earth Science, 49(3): 803-821. doi: 10.3799/dqkx.2022.096
    Citation: Qin Ya, Yang Junru, Feng Zuohai, Zhu Jiaming, Ni Zhanxu, Huang Yonggao, Wu Jie, Zhou Yun, Liu Yizhi, Bai Yuming, 2024. Mineralogy and Mineral Chemistry of the Luojiashan Gabbro in the Yingyangguan Area of Northeastern Guangxi and Its Tectonic Significance. Earth Science, 49(3): 803-821. doi: 10.3799/dqkx.2022.096
    shu

    Mineralogy and Mineral Chemistry of the Luojiashan Gabbro in the Yingyangguan Area of Northeastern Guangxi and Its Tectonic Significance

    doi: 10.3799/dqkx.2022.096
    • 1.

      Collaborative Innovation Center for Exploration of Nonferrous Metal Deposits and Efficient Utilization of Resources by the Province and Ministry & Guangxi Key Laboratory of Hidden Metallic Ore Exploration, Guilin University of Technology, Guilin 541004, China

    • 2.

      Jiangsu Tuojia Engineering Design and Research Co., Ltd., Nanjing 211100, China

    • 3.

      271 Geological Team of Guangxi Zhuang Autonomous Region, Guilin 541100, China

    • 4.

      Evaluation and Utilization of Strategic Rare Metals and Rare Earth Resource Key Laboratory of Sichuan Province & Sichuan Institute of Comprehensive Geological Survey, Chengdu 610081, China

    • Received Date: 2022-02-06
      Available Online: 2024-04-12
    • Publish Date: 2024-03-25
      Abstract
    • In this paper, the geochronology, mineralogy and mineral chemistry of Luojiashan gabbro in Yingyangguan area of northeastern Guangxi were studied, to constrain the regional tectonic background. The main mineral compositions of Luojiashan gabbro are clinopyroxene (Cpx) and plagioclase (Pl). The clinopyroxene of Luojiashan gabbro is characterized by high Fe, Al, and low Ca, Na, Ti, and its composition is Wo27-31En36-47Fs21-32, which belongs to augite. Plagioclase is characterized by high Si, Al, Na, and low Ca, K, and its composition is An0-3Ab96-100Or0-2, which belongs to albite. According to the chemical composition of clinopyroxene, the parental magma of the Luojiashan gabbro should belong to tholeiitic series. The crystallization temperature and pressure of clinopyroxene were estimated by the clinopyroxene-melt equilibrium and clinopyroxene isotherm, which yielded crystallization temperature of 1 282-1 292 ℃, with an average of 1 287 ℃. The pressures are 1.53-2.37 GPa, with an average of 2.02 GPa, and corresponding to a formation depth of 50.49-78.21 km, with an average of 66.80 km. The Luojiashan gabbro was formed at (768.9±6.8) Ma based on LA-ICP-MS zircon U-Pb dating. The chemical composition of clinopyroxene indicates that Luojiashan gabbro is a typical intraplate tholeiite. Combined with the characteristics of regional tectonic evolution, it is inferred that the Luojiashan gabbro in northeastern Guangxi originated from the extensional rift tectonic background of lithosphere thinning and mantle upwelling.

       

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