Evolution of pegmatite ore-forming fluid: The Lijiagou spodumene pegmatites in the Songpan-Garze Fold Belt, southwestern Sichuan province, China

• Published in: Ore geology reviews Vol. 139; p. 104441
• Main Authors: Fei, Guangchun, Menuge, Julian F, Chen, Changsheng, Yang, Yulong, Deng, Yun, Li, Youguo, Zheng, Luo
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.12.2021
• Subjects: Crystal-rich inclusions; Hydrothermal diamond anvil cell; Immiscibilty; Lijiagou; Pegmatite; Spodumene; Hydrothermal diamond anvil cell; Immiscibilty; Pegmatite; Spodumene; Lijiagou; Crystal-rich inclusions

[Display omitted] •Lijiagou spodumene pegmatites formed from high temperature, low salinity, volatile-enriched magmatic fluids.•Lithium enrichment occurred during fluid immiscibility.•The Lijiagou spodumene pegmatites have no direct magmatic relationship with any of the Ke'eryin plutonic rocks....