福建紫金山矿田罗卜岭斑岩型铜钼矿床辉钼矿Re-Os定年及地质意义  

Re-Os Dating of Molybdenite from the Luoboling Porphyry Cu-Mo Deposit in the Zijinshan Ore Field of Fujian Province and Its Geological Significance

作　　者：梁清玲[1] 江思宏[1] 王少怀[2] 李超[3] 曾法刚[3] 

机构地区：[1]中国地质科学院矿产资源研究所,北京100037 [2]福州大学紫金矿业学院,福州350108 [3]国家地质实验测试中心,北京100037

出　　处：《地质学报》2012年第7期1113-1118,共6页Acta Geologica Sinica

基　　金：国土资源部公益性行业科研专项(编号200911007-1-17)资助成果

摘　　要：罗卜岭铜钼矿床是位于紫金山矿田北东侧的一个大型斑岩型铜钼矿床,铜钼矿体产于四方花岗闪长岩和罗卜岭花岗闪长斑岩体内。通过对该矿床11件代表性辉钼矿样品进行Re-Os同位素定年,获得的模式年龄为104.7±1.6～106.5±1.5Ma,等时线年龄为104.9±1.6Ma,与赋矿围岩的成岩年龄一致,表明罗卜岭铜钼矿床形成于早白垩世,属燕山晚期构造-岩浆活动产物。由于斑岩铜钼矿床为紫金山矿田成矿流体早期演化的产物,故认为紫金山矿田成矿流体演化起始于105Ma左右。Located in the northeastern Zijinshan ore field, the Luoboling Cu-Mo deposit is a large-scale porphyry deposit hosted by the Sifang granodiorite and Luoboling granodiorite porphyry. Re-Os dating of eleven molybdenite separates collected from different depths of ore bodies in the Luoboling Cu-Mo deposit shows that the isochron age is 104.9±1.6 Ma and the model ages ranging from 104.7±1.6 Ma to 106.5±1.5 Ma, with an average age of 105.64±0.46 Ma. It indicates that the Luoboling Cu-Mo deposit formed in Early Cretaceous, consistent with the emplacement age of the host rocks, and that the magmatism and mineralization took place under the same geological setting. Since the Zijinshan ore field is composed of several porphyry and epithermal deposits, it is suggested that the ore fluid evolution of Zijinshan ore field may started from 105 Ma, when the Luoboling porphyry Cu-Mo deposit formed.

关 键 词：RE-OS同位素年龄 辉钼矿 成矿时代 罗卜岭铜钼矿 紫金山 

分 类 号：P618.65[天文地球—矿床学] P597.3[天文地球—地质学]