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罗卜岭铜钼矿床位于福建紫金山铜金(钼)矿田,属典型的斑岩型铜钼矿床。在罗卜岭斑岩铜钼矿床中发育的与矿化有关的成矿岩体为罗卜岭岩体,其形成时代为约103 Ma;而与矿化的无关的花岗闪长岩则发育有两期:一期早于罗卜岭岩体,形成于110 Ma;另外一期底侵早期的岩体,形成于97 Ma。罗卜岭与中寮岩体具有相似的地球化学及同位素组成,表明二者具有相同的岩浆源区。通过对罗卜岭
The Luobuling copper-molybdenum deposit is located in the Zijinshan copper-gold (molybdenum) ore field in Fujian Province and is a typical porphyry copper-molybdenum deposit. The mineralization-related ore-forming rock mass developed in the Luobuling porphyry Cu-Mo deposit is the Luobuling rock mass, which formed at about 103 Ma; while the granodiorite unrelated to mineralization developed There are two phases: one is earlier than the Luobuling rock mass and formed at 110 Ma; the other is a rock mass early at the end of an uplift formed at 97 Ma. Luobuling and Zhongliao rock mass have similar geochemical and isotopic compositions, indicating that they have the same magma source area. Through to Luo Bu Ling