幕阜山复式花岗岩体锆石年代与微量元素对伟晶岩矿床成因的限定

李安邦; 黄勤; 冯超; 杨细华; 闫刚刚; 赵子娟; 董湘杰; 祝明明; 张金阳

doi:10.3799/dqkx.2021.065

Volume 46 Issue 12

Dec. 2021

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Article Navigation > Earth Science > 2021 > 46(12): 4517-4532

Li Anbang, Huang Qin, Feng Chao, Yang Xihua, Yan Ganggang, Zhao Zijuan, Dong Xiangjie, Zhu Mingming, Zhang Jinyang, 2021. Genesis of Mufushan Pegmatite Deposits Constrained by U-Pb Ages and Trace Elements of Zircon from Complex Granitic Batholith. Earth Science, 46(12): 4517-4532. doi: 10.3799/dqkx.2021.065

Citation:

Li Anbang, Huang Qin, Feng Chao, Yang Xihua, Yan Ganggang, Zhao Zijuan, Dong Xiangjie, Zhu Mingming, Zhang Jinyang, 2021. Genesis of Mufushan Pegmatite Deposits Constrained by U-Pb Ages and Trace Elements of Zircon from Complex Granitic Batholith. Earth Science, 46(12): 4517-4532. doi: 10.3799/dqkx.2021.065

Citation:

Li Anbang, Huang Qin, Feng Chao, Yang Xihua, Yan Ganggang, Zhao Zijuan, Dong Xiangjie, Zhu Mingming, Zhang Jinyang, 2021. Genesis of Mufushan Pegmatite Deposits Constrained by U-Pb Ages and Trace Elements of Zircon from Complex Granitic Batholith. Earth Science, 46(12): 4517-4532. doi: 10.3799/dqkx.2021.065

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Genesis of Mufushan Pegmatite Deposits Constrained by U-Pb Ages and Trace Elements of Zircon from Complex Granitic Batholith

doi: 10.3799/dqkx.2021.065

1.
Hubei Nuclear Industry Geological Bureau, Xiaogan 432001, China
2.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
3.
Three Gorges Research Center for Geohazards, Ministry of Education, China University of Geosciences, Wuhan 430074, China

Received Date: 2020-12-30
Publish Date: 2021-12-15

Abstract

Abstract

Several Early Cretaceous rare metal pegmatite deposits have been discovered within and around the Late Jurassic-Early Cretaceous Mufushan complex granitic batholith in the Jiangnan metallogenic belt. It is still controversial whether the pegmatites were originated from the highly evolved Mufushan granite in this region. Tourmaline-, garnet-, and muscovite-bearing monzogranites in the Maishi and other areas have zircon LA-ICP-MS U-Pb ages between 130 and 135 Ma, similar to ages of the pegmatites within the errors. Compared with the early porphyritic biotite monzogranite and muscovite monzogranite (151-143 Ma), the late tourmaline-, garnet-, and muscovite-bearing monzogranites have zircon with high Hf, Ta, Nb, Th, U contents and low Th/U and Eu/Eu* ratios, indicating a highly evolved nature. This is also consistent with mineral assemblages and zircon crystallization temperatures of the granites. Ages and trace elements from zircon indicate that rare metal pegmatites may be the fractionated product of Early Cretaceous evolved granitic magmas in the Mufushan batholith.
- Mufushan,
- complex batholith,
- trace element of zircon,
- U-Pb dating,
- pegmatite deposit,
- petrology

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References(54)

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Genesis of Mufushan Pegmatite Deposits Constrained by U-Pb Ages and Trace Elements of Zircon from Complex Granitic Batholith

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