赣南某离子吸附型稀土矿床浅变质岩的矿化特征

赵芝; 陈郑辉; 邹新勇; 王登红; 陈振宇

doi:10.3799/dqkx.2018.297

Volume 43 Issue 10

Oct. 2018

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Zhao Zhi, Chen Zhenghui, Zou Xinyong, Wang Denghong, Chen Zhenyu, 2018. REE Mineralization of Epimetamorphic Rocks from an Ion-Adsorption Type REE Deposit in Southern Jiangxi Province. Earth Science, 43(10): 3652-3663. doi: 10.3799/dqkx.2018.297

Citation:

Zhao Zhi, Chen Zhenghui, Zou Xinyong, Wang Denghong, Chen Zhenyu, 2018. REE Mineralization of Epimetamorphic Rocks from an Ion-Adsorption Type REE Deposit in Southern Jiangxi Province. Earth Science, 43(10): 3652-3663. doi: 10.3799/dqkx.2018.297

Citation:

Zhao Zhi, Chen Zhenghui, Zou Xinyong, Wang Denghong, Chen Zhenyu, 2018. REE Mineralization of Epimetamorphic Rocks from an Ion-Adsorption Type REE Deposit in Southern Jiangxi Province. Earth Science, 43(10): 3652-3663. doi: 10.3799/dqkx.2018.297

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REE Mineralization of Epimetamorphic Rocks from an Ion-Adsorption Type REE Deposit in Southern Jiangxi Province

doi: 10.3799/dqkx.2018.297

1.
MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
Geological Survey Team of Gannan, Bureau of Geology and Mineral Exploration & Development of Jiangxi Province, Ganzhou 341000, China

Received Date: 2017-05-09
Publish Date: 2018-10-20

Abstract

Abstract

An ion-adsorption type REE deposit occurs in regolith of epimetamorphic rocks formed in Neo-Proterozoic, and has been discovered in South Jiangxi Province in recent years. Petrological and geochemical characteristics of the rocks from the REE deposit and Nanling scientific drilling were studied in this paper. Shenshan Formation and Kuli Formation are widely exposed in the deposit, and the former consists mainly of phyllite and minor schist whereas the latter consists of thick-layer metatuffite, metamorphic tuff, and medium-thick-layer metasandstone. Kuli Formation is composed of metamorphic tuff with thin layer tuffaceous slate that intersected by Nanling scientific drilling from 1 165 m to 1 170.77 m. The epimetamorphic rocks with neo formation of sericite, chlorite, magnetite, cordierite, muscovite, biotite, etc. contain REE minerals such as synchysite-(Ce), monazite, xenotime and rhabdophane-(La) etc. They are enriched in REEs (162×10^-6 to 723×10^-6) with high LREE/HREE ratios (LREE/HREE=2-7).We suggest that Ion-adsorbed REEs in the regolithic zone of the epimetamorphic rocks are mainly sourced from REE-fluorocarbonate. Regolith of metamorphic tuff and metatuffite formed in Cryogenian in South Jiangxi Province should be included during REE-bearing properties evaluation and prospecting.
- epimetamorphic rock,
- rare earth elements,
- ion-adsorption REE deposit,
- South Jiangxi Province,
- mineral deposits

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References(61)

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