Generation of Late Mesozoic Qianlishan A2-type granite in Nanling Range, South China: Implications for Shizhuyuan W-Sn mineralization and tectonic evolution
The Qianlishan complex is an A2-type granite, formed at ~ 158–154 Ma induced by slab rollback. The A2 signature of the Qianlishan granite indicates mantle metasomatism during plate subduction. Fractionation of reduced granitic melts and melt–fluid interaction account for the formation of Shizhuyuan W–Sn deposit.