福建上杭罗卜岭铜钼矿床中侵入岩的矿物学研究及成矿意义
摘要
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。
出处
《矿物学报》
CAS
CSCD
北大核心
2015年第S1期30-,共1页
Acta Mineralogica Sinica
基金
国家科技部973项目(2012CB416706)
中南大学‘创新驱动计划’项目(2015CX008)
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