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研究背景: 北方东部复合造山带经历古亚洲洋构造体制的增生过程,又遭受蒙古-鄂霍茨克洋和古太平洋构造体制的叠加与改造,形成独具特色的俯冲增生斑岩铜-金-钼矿和陆壳再造银-铅-锌-钨-锡-钼矿床共存的复合成矿省,具有“三大构造体制,两向汇聚叠加”和“三大成矿系统,多期复合成矿”的鲜明特征,明显不同于北方西部增生造山带。本项目立足于复合造山与叠加成矿这一核心科学问题,以标志性复合成矿系统深部结构和典型矿集区为研究重点,揭示复合造山成矿系统的深部结构与成矿“末端”...