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Shi, Aiguo, Xu, Cheng, Fan, Chaoxi, Chakhmouradian, Anton R., Brenna, Marco, Wei, Chunwan (2024) Structural Defects of Heavy Rare Earth Element Minerals in Granite Accelerate Their Decomposition and Facilitate Mineralization During Weathering. Economic Geology, 119 (4) 871-883 doi:10.5382/econgeo.5057

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Reference TypeJournal (article/letter/editorial)
TitleStructural Defects of Heavy Rare Earth Element Minerals in Granite Accelerate Their Decomposition and Facilitate Mineralization During Weathering
JournalEconomic Geology
AuthorsShi, AiguoAuthor
Xu, ChengAuthor
Fan, ChaoxiAuthor
Chakhmouradian, Anton R.Author
Brenna, MarcoAuthor
Wei, ChunwanAuthor
Year2024 (June)Volume<   119   >
Issue<   4   >
URL
DOIdoi:10.5382/econgeo.5057Search in ResearchGate
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Mindat Ref. ID17432749Long-form Identifiermindat:1:5:17432749:5
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Full ReferenceShi, Aiguo, Xu, Cheng, Fan, Chaoxi, Chakhmouradian, Anton R., Brenna, Marco, Wei, Chunwan (2024) Structural Defects of Heavy Rare Earth Element Minerals in Granite Accelerate Their Decomposition and Facilitate Mineralization During Weathering. Economic Geology, 119 (4) 871-883 doi:10.5382/econgeo.5057
Plain TextShi, Aiguo, Xu, Cheng, Fan, Chaoxi, Chakhmouradian, Anton R., Brenna, Marco, Wei, Chunwan (2024) Structural Defects of Heavy Rare Earth Element Minerals in Granite Accelerate Their Decomposition and Facilitate Mineralization During Weathering. Economic Geology, 119 (4) 871-883 doi:10.5382/econgeo.5057
InLink this record to the correct parent record (if possible)
Abstract/NotesHeavy rare earth elements (HREEs), an indispensable resource for modern industry, are extracted mainly from clays in ion adsorption deposits (IADs) in South China. The HREEs in IADs are derived from accessory minerals in parental granites. These precursor HREE phases have low solubility in aqueous environments, and unraveling the mechanism of their decomposition during weathering is critical to understanding how IADs form. Here, we report the micro- to nanoscale structural characteristics of HREE precursor minerals in parental granites from the large Zudong and Zhaibei IADs. High-resolution transmission electron microscopy shows that these minerals are characterized by abundant structural defects that range from lattice dislocations to submicro- to nanoscale crystallite aggregates with a variable proportion of amorphous material. Ubiquitous structural defects make the precursor HREE minerals unstable during weathering, resulting in their rapid decomposition, thereby facilitating the development of clay-hosted mineralization.

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LocalityCitation Details
Zhaibei deposit, Dingnan Co., Ganzhou, Jiangxi, China
Zudong Mine, Longnan REE deposits, Longnan Co., Ganzhou, Jiangxi, China

Mineral Occurrences

LocalityMineral(s)
Zhaibei deposit, Dingnan Co., Ganzhou, Jiangxi, Chinaⓘ Bastnäsite-(Ce), ⓘ Bastnäsite-(La), ⓘ Biotite, ⓘ Biotite granite, ⓘ Cerianite-(Ce), ⓘ Churchite-(Y), ⓘ Eudialyte, ⓘ Feldspar Group, ⓘ Fergusonite-(Y), ⓘ Fluorapatite, ⓘ Fluorite, ⓘ Gadolinite, ⓘ Gadolinite-(Y), ⓘ Granite, ⓘ Granitoid, ⓘ Halloysite, ⓘ Kaolinite, ⓘ Monazite Group, ⓘ Monazite-(Ce), ⓘ Muscovite, ⓘ Muscovite granite, ⓘ Plagioclase, ⓘ Quartz, ⓘ Regolith, ⓘ Rhabdophane, ⓘ Rhabdophane-(Y), ⓘ Synchysite-(Ce), ⓘ Synchysite-(Y), ⓘ Thorite, ⓘ Xenotime, ⓘ Xenotime-(Y), ⓘ Xenotime-(Yb), ⓘ Zircon
Zudong Mine, Longnan REE deposits, Longnan Co., Ganzhou, Jiangxi, Chinaⓘ Apatite, ⓘ Biotite, ⓘ Feldspar Group, ⓘ Fergusonite-(Y), ⓘ Fluorite, ⓘ Gadolinite, ⓘ Gadolinite-(Y), ⓘ Granite, ⓘ Halloysite, ⓘ Kaolinite, ⓘ Muscovite, ⓘ Muscovite granite, ⓘ Plagioclase, ⓘ Quartz, ⓘ Synchysite, ⓘ Synchysite-(Ce), ⓘ Synchysite-(Y), ⓘ Thorite, ⓘ Xenotime, ⓘ Xenotime-(Y), ⓘ Xenotime-(Yb), ⓘ Zircon


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