2022 Vol. 49, No. 1
Article Contents

ZHANG Min, HE Xianchuan, TAN Wei, MA Lingya, ZHAO Fufeng. 2022. Geochemical characteristics and genesis of ion-adsorption type REE deposit in the Lincang granite, Yunnan Province[J]. Geology in China, 49(1): 201-214. doi: 10.12029/gc20220112
Citation: ZHANG Min, HE Xianchuan, TAN Wei, MA Lingya, ZHAO Fufeng. 2022. Geochemical characteristics and genesis of ion-adsorption type REE deposit in the Lincang granite, Yunnan Province[J]. Geology in China, 49(1): 201-214. doi: 10.12029/gc20220112

Geochemical characteristics and genesis of ion-adsorption type REE deposit in the Lincang granite, Yunnan Province

    Fund Project: Supported by Guangdong Major Project of Basic and Applied Basic Research(No. 2019B030302013); the 2020 open fund of Guangdong Provincial Key Laboratory of Mineral Physics and Materials (Science and Technology Planning Project of Guangdong Province, China)(No. 2020B1212060055); Investigation and Evaluation of Fubang Rare Earth Mine in Lancang, Yunnan (DD20160016-19) about Chengdu Center of China Geological Survey
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  • Author Bio: ZHANG Min, male, born in 1986, master, geological engineer, engaged in mineral deposit geochemistry research and solid mineral exploration; E-mail: zhangmin1179@126.com
  • This paper is the result of mineral exploration engineering.

    Objective

    The widespread Lincang granite weathering crust has the enormous potential of ion-adsorption type REE resource. Strengthening the research on the phase characteristics and leaching rate of ion-adsorption type REE deposit in Lincang granite weathering crust and other ore deposit geochemical characteristics and metallogenic mechanisms will help to further promote the prospecting of ion-adsorbed rare earth resources in this area.

    Methods

    Through systematic drilling projects in the middle section of Lincang granite, a detailed understanding of rare earth metallogenic geology and ore deposit geochemical characteristics, and its genesis are discussed.

    Results

    All-phase and leaching-phase of REE in the full weathering layer of crust are strongly differentiated, their distribution patterns show "W" shapes as smooth and shallow; the ores are the mixed type of LREE-enriched; REE ore bodies lay in the full weathering layer of granite weathering crust, and grade changes from top to bottom show two types as " low- high" and " high- low".

    Conclusions

    The infiltrating acidic solution carries the REE which dissociate from the sub-minerals of granite migrating down, the REE enrich and mineralize in the full weathering layer of crust, because the clay minerals and acidic solutions declined sharply, the enrichment of half weathered layer and weak weathered layer are greatly reduced.

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