Abstract
Highly evolved granites can be important hosts of rare earth element (REE) resources, and more importantly, they commonly serve as the protolith for regolith-hosted REE deposits to form during weathering. Highly evolved granites in the Zudong pluton, South China, are extremely rich in the heavy (H)REE (up to 8000 ppm total HREE), and display significant REE fractionation. Moreover, the HREE enrichment is positively correlated with the degree of REE fractionation, indicating a unique process in preferentially enriching the HREE during the evolution of the granites. Multiple stages of hydrothermal re-mobilization of the REE can account for the HREE mineralization, and these are recorded in the texture and composition of the zircon. In these processes, fluctuations in the F activity of the fluid caused alternating dissolution-reprecipitation and continuous growth of the zircon. REE were repeatedly mobilized and enriched in the fluid to precipitate the major HREE mineral synchysite-(Y), and partially incorporated into the growth zone of zircon, while other elements were largely lost to the fluid during the extensive dissolution of the rock-forming minerals. LREE were also likely substantially mobilized in the late hydrothermal stage and lost through complexation with Cl, causing the significant LREE depletion and, thus REE fractionation. This process continuously enriched host granites in the HREE to a potentially economic grade, making them favorable protoliths for subsequent supergene regolith-hosted HREE deposits.
Acknowledgments and Funding
We thank Xiao Fu for the support on XRF and EPMA analyses. Editorial handling and comments by Associate Editor Paul Tomascak and constructive reviews by El Saeed R. Lasheen and an anonymous reviewer are very much appreciated. This study was supported financially by the Natural Science Foundation of China (Grant No. 92162323, 91962216) and the Guangdong Basic and Applied Basic Research Foundation (Grant No. 2021A1515011524) to M.-F.Z.
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Articles in the same Issue
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Articles in the same Issue
- Tetrahedral aluminum in tourmaline from a spinel-pargasite-metamorphosed mafic-ultramafic rock
- Lorenz number and transport properties of Fe: Implications to the thermal conductivity at Earth’s core-mantle boundary
- Structure and equation of state of Ti-bearing davemaoite: New insights into the chemical heterogeneity in the lower mantle
- Solfataric alteration at the South Sulfur Bank, Kilauea, Hawaii, as a mechanism for the formation of sulfates, phyllosilicates, and silica on Mars
- Plastic deformation and trace element mobility in sphalerite
- Crystallographic insights into monovalent thallium incorporation: Exploring hydropyrochlore structure for environmental remediation
- Distribution of REE between amphibole and pyroxenes in the lithospheric mantle: An assessment from the lattice strain model
- Elastic anomalies across the P21nm→Pnnm structural phase transition in δ-(Al,Fe)OOH
- Hyper-enrichment of heavy rare earth elements in highly evolved granites through multiple hydrothermal mobilizations
- In-situ zircon and cassiterite LA-ICP-MS geochronology and implications for granite-hosted Sn deposit models and exploration: Insights from the Cameroon Line
- Compressibility, thermal expansion, and Raman spectroscopy of synthetic whitlockite Ca9Mg(PO3OH)(PO4)6 at high pressures and high temperatures
- Experimental determination of tin partitioning between titanite, ilmenite, and granitic melts using improved capsule designs
- Low-temperature crystallization of kumdykolite, a polymorph of albite, during mineral carbonation within fluid inclusions in hornblendite from the Dabie orogen, central China
- Louisfuchsite, Ca2(Mg4Ti2)(Al4Si2)O20, a new rhönite-type mineral from the NWA 4964 CK meteorite: A refractory phase from the solar nebula