Geology and Molybdenite Re-Os Ages of Makeng Skarn-Type Fe-Mo Deposit in Fujian ProvinceChinese Full Text
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
Abstract: 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 Cr... More
- DOI:
10.13278/j.cnki.jjuese.2012.s1.024
- Series:
(A) Mathematics/ Physics/ Mechanics/ Astronomy; (B) Chemistry/ Metallurgy/ Environment/ Mine Industry
- Subject:
Geology; Mining Engineering
- Classification Code:
P618.65;P597.3
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