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    Volume 47 Issue 4
    Apr.  2022
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    Article Navigation >  Earth Science  > 2022  >  47(4): 1383-1398
    Liang Xiao, Xu Yajun, Zi Jianwei, Zhang Hangchuan, Du Yuansheng, 2022. Genetic Mineralogy of Monazite and Constraints on Interpretation of U-Th-Pb Ages. Earth Science, 47(4): 1383-1398. doi: 10.3799/dqkx.2021.157
    Citation: Liang Xiao, Xu Yajun, Zi Jianwei, Zhang Hangchuan, Du Yuansheng, 2022. Genetic Mineralogy of Monazite and Constraints on Interpretation of U-Th-Pb Ages. Earth Science, 47(4): 1383-1398. doi: 10.3799/dqkx.2021.157
    shu

    Genetic Mineralogy of Monazite and Constraints on Interpretation of U-Th-Pb Ages

    doi: 10.3799/dqkx.2021.157
    • 1.

      School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

    • 2.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

    • Received Date: 2021-05-12
      Available Online: 2022-04-29
    • Publish Date: 2022-04-25
      Abstract
    • Monazite U-Pb geochronology plays an important role in dating magmatism, metamorphism and sedimentation. Because of its complex genesis, characterizing different types of monazite in terms of genetic mineralogy and chemistry is of great significance to interpret geochronology data. In this paper, it summarizes the occurrence (mineral paragenesis), crystal morphology and mineral geochemistry of different monazite in origins. The results show that magmatic monazite has straight edges, angular or embayment shape, showing oscillatory zoning, sector zoning and homogeneous internal structure, generally existing as inclusions that coexisting with feldspar and quartz. Metamorphic monazite is divided into high-grade and low-grade types. High-grade metamorphic monazite has straight edges, with concentric zoning, patchy zoning and intergrowth-like zoning or unzoned, generally associated with metamorphic porphyroblast (such as garnet). Low-grade metamorphic monazite occurs as discrete crystals with numerous inclusions, commonly exhibiting skeletal texture. Hydrothermal monazite has two types: the first type occurs as a cluster of multiple small monazite grain (< 50 μm) and the other type is grains showing oscillatory zoning and sector zoning. The rare earth element pattern of monazite is commonly right-leaning. Magmatic monazite has the strongest negative Eu anomalies with high Th, U, Pb, Y and HREE contents. High-grade metamorphic monazite has moderate negative Eu anomalies with high Th, U; HREE and Y are correlated with its coexisting minerals, whereas low-grade metamorphic monazite has insignificant negative Eu with low Th and U. Hydrothermal monazite has weak negative Eu, extremely low U and high Th/U ratio.

       

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