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Geochronology and genesis of rare-metal mineralization in the Himalayan leucogranite-pegmatite system
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DOI:10.1016/j.lithos.2026.108702.png)
Abstract
En 中文
• U-Pb ages reveal multi-pulse Himalayan rare-metal pegmatite events. • Apatite trace elements record high ƒO2, fluid exsolution, and extreme differentiation. • Apatite δ18O distinguishes three fluid evolution types in Himalayan leucogranites.
Journal
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2.5
Papers:
649
Citations:
2.8W
