High-Temperature Vibrational Analysis of the Lithium Mica: 2M2 Lepidolite

• Published in: Minerals (Basel) 2023-09, Vol.13 (9), p.1112
• Main Authors: Zhang, Ziyu, Cheng, Hang, Zhang, Li, Li, Xiaoguang, Lu, Xiaofeng, He, Haoxiong, Zhang, Zhuoran, Chen, Tianze
• Format: Article
• Language: English
• Subjects: Aluminum; Cooling; Crystal structure; Data collection; Dehydration; Electron microprobe; Electron probes; Electrons; Geology; Geophysics; Heating; High temperature; high-temperature infrared spectroscopy; high-temperature Raman spectroscopy; Hydrogen ions; hydroxyl; lepidolite; Lithium; Mica; Oxygen; Pegmatite; Rubidium; Silicates; Single crystals; Slabs; Subduction; Subduction (geology); Subduction zones; Temperature; Thermal response; trioctahedral mica; Vibrational analysis; X-ray diffraction
• ISSN: 2075-163X; 2075-163X
• DOI: 10.3390/min13091112

Lepidolite is widespread in the upper crust and can be used as a lithium ore. In the present study, in-situ high-temperature Raman and infrared spectroscopic measurements of natural Rb/Cs-free 2M2 lepidolite in pegmatite were conducted up to 700 °C for investigating the thermal response of lepidolite. In addition, single-crystal X-ray diffraction and electron microprobe analyses were also conducted to determine the polytype and composition of the lepidolite sample. The results show that (1) in the temperature range from 25 to 700 °C, the crystal structure of 2M2 lepidolite is not expected to undergo remarkable transformations upon heating and cooling; (2) the stabilities of hydroxyls in high-charge environments are lower than those in low-charge environments at elevated temperatures up to 700 °C. As a result, hydrogen ions in 2M2 lepidolite can transfer from the non-silicate oxygens in high-charge environments to those in low-charge environments during heating; (3) the transfers of the hydrogen ions between non-silicate oxygens in high-charge and low-charge environments may lead to the dehydration of lepidolite. Thus, lepidolites in subduction zones at temperatures below 700 °C can be sufficient to trigger partial melting and result in the release of lithium in subducted oceanic and continental slabs during subduction and exhumation.