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Supplemental Material: Multistage magmatic-hydrothermal processes formed world-class granite-related lithium mineralization at Yifeng-Fengxin, South China: Evidence from zircon mineralogy
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<p>Figure S1: Photomicrographs of the ore-hosting granitic complex. (A) Porphyritic biotite granite; (B) two-mica granite; (C) muscovite granite; (D) muscovite syenogranite; (E) zinnwaldite granite; (F) lepidolite granite. Figure S2: Natural logarithmzircon/melt versus lattice-strain parameter for REE3+ for multiphase granites in the Yifeng-Fengxin Li deposit. (III—cations equation from Nd to Lu; IV—cations equation for Th, U, Hf, and Zr). Table S1: LA-ICP-MS U-Pb dating results for zircons from different granite phases in the Yifeng-Fengxin Li deposit. Table S2: In situ trace elements for zircons from different granite phases in the Yifeng-Fengxin Li deposit. Table S3: In situ Hf isotopic results for zircons from different granite phases in the Yifeng-Fengxin Li deposit.</p>
Title: Supplemental Material: Multistage magmatic-hydrothermal processes formed world-class granite-related lithium mineralization at Yifeng-Fengxin, South China: Evidence from zircon mineralogy
Description:
<p>Figure S1: Photomicrographs of the ore-hosting granitic complex.
(A) Porphyritic biotite granite; (B) two-mica granite; (C) muscovite granite; (D) muscovite syenogranite; (E) zinnwaldite granite; (F) lepidolite granite.
Figure S2: Natural logarithmzircon/melt versus lattice-strain parameter for REE3+ for multiphase granites in the Yifeng-Fengxin Li deposit.
(III—cations equation from Nd to Lu; IV—cations equation for Th, U, Hf, and Zr).
Table S1: LA-ICP-MS U-Pb dating results for zircons from different granite phases in the Yifeng-Fengxin Li deposit.
Table S2: In situ trace elements for zircons from different granite phases in the Yifeng-Fengxin Li deposit.
Table S3: In situ Hf isotopic results for zircons from different granite phases in the Yifeng-Fengxin Li deposit.
</p>.
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