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Li-rich pegmatites are commonly associated with evolved magmatic suites in post-collisional settings with significant mantle input, yet the petrogenetic links between mantle-derived magmatism and crustal felsic melts remain poorly constrained. The Ke’eryin intrusive complex, located in the eastern Songpan–Ganze Orogenic Belt (SGOB), offers a rare opportunity to reconstruct the complete magmatic evolution from the emplacement of mantle-derived mafic melts to highly evolved spodumene-bearing pegmatites that host world-class lithium (Li) mineralization.

Petrogenesis and Lithium Mineralization of the Ke’eryin Diorite–Granite–Spodumene Pegmatite Complex in the Songpan-Ganze Orogenic Belt (China)