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Lithium Isotope Fractionation in Tibet Pegmatites by Soh Ail Gaming is a document available to read on EtoBox.

What is Lithium Isotope Fractionation in Tibet Pegmatites about?

This study investigates lithium isotope fractionation in the Bailongshan pegmatites of NW Tibet, revealing two types of pegmatites: Li-poor and Li-rich. The findings suggest that these pegmatites formed from melt-fluid separation during granitic magma evolution, with distinct isotopic compositions indicating different fluid environments. The research highlights the role of supercritical fluid exsolution in Li mineralization and the geochemical behavior of lithium isotopes in pegmatite systems.

Author
Soh Ail Gaming
Language
EN