Genesis of REE minerals in the karstic bauxite in western Guangxi,China, and its constraints on the deposit formation conditions |
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| Institution: | 1. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China;2. The Bureau of Geo-exploration Guangxi and Mineral Development, Nanning 530023, China;1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, PR China;2. Institute of Multipurpose Utilization of Mineral Resources, Chinese Academy of Geological Sciences, Chengdu 610041, PR China;3. State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, PR China;4. Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, PR China;5. Chengdu Institute of Geology and Mineral Resources, Geological Survey of China, Chengdu 610081, PR China;1. Department of Earth Science, Faculty of Sciences, University of Kurdistan, Sanandaj 66177-15175, Iran;2. Department of Sciences, University of Basilicata, viale dell''Ateneo Lucano 10, 85100 Potenza, Italy;1. Department of Sciences, University of Basilicata, viale dell''Ateneo Lucano 10, 85100 Potenza, Italy;2. CNR — Istituto di Metodologie per l''Analisi Ambientale, c/da S. Loya, 85050, Tito Scalo, Italy;3. CNR — Istituto di Geoscienze e Georisorse, via Ferrara 1, 27100 Pavia, Italy |
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| Abstract: | Karstic bauxites in western Guangxi, China, comprise two subtypes: Permian bauxite and Quaternary bauxite. The Quaternary bauxite originated from the breaking up, rolling, and accumulating of Permian bauxite in karstic depressions in Quaternary. Various types of rare earth element (REE) minerals were discovered during the formation of the Permian and Quaternary bauxites from the Xinxu, Longhe, and Tianyang bauxite deposits in this study. Five types of REE minerals, including bastnäsite, parisite, cerianite, rhabdophane, and churchite, were identified. Bastnäsite and parisite are the most abundant, and they are widely developed in the Permian ore and also present in the Quaternary ore. Obvious variations in bastnäsite and parisite REE compositions were observed, which is ascribed to distinctions in the source materials in the primary weathering profile from different areas. The mode of occurrence of bastnäsite and parisite suggests they were mainly precipitated under alkaline and reducing conditions during the Permian bauxite-forming stage and underwent intensive corrosion in the Quaternary. Churchite was formed during the Permian weathering stage under acidic condition. Both cerianite and rhabdophane occur in fractures within the Permian bauxite ore, indicating that both formed during the Quaternary weathering stage. It is considered that the rhabdophane enriched in Ce have formed locally, in the process of that the Ce3 +, released from bastnäsite rapidly, entered the rhabdophane lattice before being oxidized to Ce4 +. Cerianite was mainly found in association with Mn–Al hydroxides, suggesting that the released Ce3 + was oxidized into Ce4 + and precipitated cerianite in fractures within the Permian bauxite ore. Mass balance equations reveal a depletion in nearly all REEs during the transformation from the Permian to the Quaternary bauxite ore, mainly caused by the dissolution of bastnäsite and parisite. The genesis of the REE minerals, together with the occurrence of other minerals, indicates that intensively acidic and oxidizing conditions developed before the formation of the Permian bauxite ore. Towards the end of the Permian, the conditions became reducing and alkaline, favorable for the large-scale bauxitization. The Quaternary bauxite-forming stage was characterized by variable pH and Eh conditions, with acidic (pH = 4–6) and oxidizing (Eh > 2) conditions at the surface of the exposed Permian bauxite ore. |
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