HANDBOOK ON THE PHYSICS AND CHEMISTRY OF RARE EARTHS

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HANDBOOK ON THE PHYSICS AND CHEMISTRY OF RARE EARTHS ( handbook-onphysics-and-chemistry-rare-earths )

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REE Mineralogy and Resources Chapter Weakly Strongly Metaluminous peraluminous peraluminous 1.5 1.4 1.3 1.2 1.1 1.0 0.9 0.8 0.8 0.9 1.0 1.1 1.2 1.3 1.4 1.5 Molar Al2O3/(CaO + Na2O + K2O) 279 209 FIG. 39 Zudong muscovite granite (Longnan) Zudong biotite granite (Longnan) Guanxi biotite granite (Longnan) Muscovite granite (Datian) Biotite granite (Datian) (Biotite-)muscovite granite (Zhaibeiding) Biotite granite porphyry (Heling) Rhyolite (Heling) Biotite granite (Dingnan) Biotite granodiorite (Dajishan) Biotite granite (Laishi) Biotite granite porphyry (Renju) Biotite granite (Renju) Biotite granite (Huashan) Biotite granite (Guposhan) Plots of molar Al2O3/(Na2O + K2O) vs Al2O3/(CaO + Na2O + K2O) ratios of parent rocks underlying the ion-adsorption ore bodies in southern China. pyrite (Wu et al., 1993b; Table 13). The ion-adsorption ores show REE grades from 131 to 589 ppm and LaN/YbN ratios from 0.23 to 1.5 (Ma et al., 1991; Wu et al., 1993b), which suggest strong enrichment in HREE (Figs. 40F,G and 41D). The LREE-rich Heling deposits are located in Xunwu County of Jiangxi Province. A weathering profile is mainly developed on the Heling granite por- phyry, which is surrounded by rhyolitic lava and tuff. The granite porphyry has high alkali (Na2O+K2O) contents (Bao and Zhao, 2008; Song and Shen, 1986; Yang et al., 1981; Zhang, 1990) compared to calc-alkaline gran- ites in other deposits, suggesting a low degree of partial melting. The REE content of the granite porphyry is 808 ppm, significantly higher than those of calc-alkaline granites associated with other deposits. The Heling granite are enriched in LREEs and depleted in HREEs and are predominantly contained in bastnäsite-(Ce) and apatite with subdominant in zircon, mona- zite, fergusonite, and synchysite-(Y). The ion-adsorption ores of Heling show high REE grade ranging widely from 510 to 6460 ppm, and high LaN/YbN ratios of 42–121 compared to the Longnan ores, because the underlying parent rocks were originally rich in REEs (particularly in LREEs; Fig. 41F). Molar Al2O3/(Na2O + K2O) Peralkaline

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