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《Journal of Jilin University(Earth Science Edition)》 2012-S1
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Geology and Molybdenite Re-Os Ages of Makeng Skarn-Type Fe-Mo Deposit in Fujian Province

Zhang Cheng-shuai1,Mao Jing-wen2,Xie Gui-qing2,Zhao Cai-sheng3, Yu Miao1,Wang Jin-xiang4,Liu Wu-gang4 1.Faculty of Sciences and Mineral Resources,China University of Geosciences,Beijing 100083,China 2.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China 3.Technology and International Cooperation Department,Ministry of Land and Resources,Beijing 100812,China 4.Makeng Mining Company Limited,Fujian,Longyan 364021,Fujian,China  
Makeng Fe-Mo deposit is a large strata-bound skarn-type deposit occurred in the exo-contact zone of the Juzhou-Dayang granite and hosted by interbedfaults between Huanglong Formation(C2h) carbonates and Lindi Formation(C1l) clastic rocks.Seven molybdenite samples separated from the Makeng skarn ore bodies were used for Re-Os dating.The obtained the model ages range from(131.9±1.9) Ma to(133.3±2.3) Ma,averaging at(133.0±0.8) Ma,indicating that the major metallogenic stage occurred at the Early Cretaceous,which is consistent with the emplacing age of the host rock Juzhou granitic pluton.Our results suggest that they are products of the same epoch magma,structure,and fluid activities.Five out of seven molybdenite samples show Re contents at 0.47×10-6~5.14 ×10-6,and the other two at 51.87×10-6 and 186.2×10-6,respectively.Combined with fact that the Juzhou-Dayang pluton are the crust-derived granite,we infer that the ore-forming material mainly derived from upper crust with minor addition from the mantle.The metallogenic epoch of Makeng Fe-Mo deposit may consider as the response to the Late Mesozoic regional lithospheric thinning in the South China block.
【Fund】: 国家自然科学重点基金项目(40930419);; 中央高校基本科研业务费专项资金项目(2011PY0158)
【CateGory Index】: P618.65;P597.3
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