HOU Man-tang, YAN Zhen, GAO Huai-xiong. Mineralization, Geological Features, and Prospecting Indicators of the Copper(Molybdenum) in Southern Margin of Taibai Rock-Mass[J]. Northwestern Geology, 2010, 43(1): 75-85.
Citation: |
HOU Man-tang, YAN Zhen, GAO Huai-xiong. Mineralization, Geological Features, and Prospecting Indicators of the Copper(Molybdenum) in Southern Margin of Taibai Rock-Mass[J]. Northwestern Geology, 2010, 43(1): 75-85.
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Mineralization, Geological Features, and Prospecting Indicators of the Copper(Molybdenum) in Southern Margin of Taibai Rock-Mass
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1.
Geological Survey of Shaanxi Province, Xi'an 710054, Shaanxi, China
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2.
Geological Institute of Geology Chinese Academy of Sciences, Beijing 100037, China
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Abstract
In the southern margin Taibai rock-mass,the copper(molybdenum)ore has been found.There are 2 copper ore bodies,one copper-based body and 5 molybdenum mineralized bodies.The length of the Copper ore body is 245~445 m,with an average thickness of 2.03~2.81 m and an average grade of 1.57% to 1.67%.The length of molybdenum mineralized body is 50m,with a thickness of 2.03~2.81 and a grade of 0.01%~0.54%.The mineralizattion of copper-molybdenum is controlled by three factors: rock,structure,and alteration.We use the mining ore molybdenite Re-Os method to testiso topic age and obtain the age of 119.3~123.7 Ma for the copper-molybdenum mineralization in this area formed in the late Yanshan. In the southern margin Taibai rock-mass,the copper(molybdenum)ore has been found.There are 2 copper ore bodies,one copper-based body and 5 molybdenum mineralized bodies.The length of the Copper ore body is 245~445 m,with an average thickness of 2103~2181 mand an average grade of 1.57% to 1.67%.The length of molybdenum mineralized body is 50m,with a thickness of 2.03~2.81m and a grade of 0.01%~0.54%.The mineralizattion of copper-molybdenum is controlled by three factors: rock,structure,and alteration.We use the mining ore molybdenite Re-Os method to test isotopic age and obtain the age of 119.3~123.7 Ma for the copper-molybdenum mineralization in this area formed in the late Yanshan.
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