Indicative Significance of the Characteristics of Kumusayi Pegmatite in Ruoqiang County for the formation of Lithium Deposits
The research area is located in the Altun Copper Gold Metallogenic Belt on the northern edge of the Qinghai Tibet Plateau,situated between the Qaidam block,the Qilian-Kunlun orogenic belt,and the Tarim block.The Kumusayi granite pegmatite type lithium deposit in Ruoqiang County has a high degree of differentiation,and the light and heavy rare earth components are not obvious.It may be derived from partial melting of crustal materials,and the tectonic envi-ronment is a subduction environment caused by the rotation of the North Altun Ocean.By studying the geological charac-teristics,genesis,and resource potential of the Kumusayi granite pegmatite type lithium deposit,this study provides guid-ance for searching for similar lithium resources in the Altun region.
Altyn orogenic beltHighly differentiated pegmatiteLithium polymetallic deposit
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