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논문 기본 정보

자료유형
학술저널
저자정보
Xiao Nie (Institute of Mineral Resources Chinese Academy of Geological Sciences) Zong-qi Wang (Institute of Mineral Resources, Chinese Academy of Geological Sciences) Lei Chen (Institute of Mineral Resources Chinese Academy of Geological Sciences) Jingwu Yin (China University of Geosciences) Gang Wang (Institute of Mineral Resources, Chinese Academy of Geological Sciences)
저널정보
한국지질과학협의회 Geosciences Journal Geosciences Journal Vol.25 No.5
발행연도
2021.10
수록면
605 - 617 (13page)
DOI
10.1007/s12303-020-0062-3

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초록· 키워드

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In recent years, several Nb-rare-earth-element (REE) deposits have been discovered in trachyte from the Pingli?Zhenping area of the North Daba Mountain. Of these, the Zhujiayuan Nb (-REE) deposit is particularly rich in monazite. In this study, electron probe microanalysis (EPMA) and laser-ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) were used to better understand the genesis of the deposit and constrain the timing of Nb-REE mineralization. The results show that most monazite in the deposit is closely related to various alteration minerals (biotite, sericite, albite, quartz, pyrite, and calcite), and monazite often has a lower ThO2 content (0.09?1.32 wt%), indicating its hydrothermal origin. Monazite and the dominant Nb-bearing mineral (columbite) have a close paragenetic relationship, indicating that Nb and REE were mineralized in the same period. LA-ICP-MS U-Pb dating on hydrothermal monazite grains shows a weighted average 206Pb/238U age of 237.2 ± 7.9 Ma, which represents the timing of REE mineralization. The origin of monazite, in combination with the alteration mineralogy and ore-forming age, suggests that fluid exsolved from the Early Mesozoic alkaline felsic melt induced widespread hydrothermal alteration and the formation of the Zhujiayuan Nb-REE deposit.

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