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《Geotectonica et Metallogenia》 2015-02
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Zircon U-Pb Dating of Intermediate-Acid Intrusive Rocks in the Middle Section of Ningzhen District and Their Metallogenic Implications

GUAN Junpeng;WEI Fubiao;SUN Guoxi;HUANG Jianping;WANG Lijuan;Geological Survey of Jiangsu Province;  
The Ningzhen metallogenic district is an important part of the Middle-Lower Yangtze River Valley metallogenic belt. LA-ICP-MS zircon U-Pb dating of the three intermediate-acid intrusions, i.e., Anjishan, Xinqiao, and Shima, in the central part of the Ningzhen district, indicates that those intrusions were emplaced in the Late Early Cretaceous, with ages of 107.0±1.1 Ma–108.0±1.6 Ma, 108.0±1.3 Ma, and 102.5±1.1 Ma, respectively. Combined with the molybdenite Re-Os isotope age(106–108 Ma) of porphyry copper deposit in this regions, the Ningzhen district exists an intensively magmatic-metallogenic-thermal event at 102.5–108.0 Ma. The age of this event is similar with the age of the third period of large scale mineralization in South China, however obviously later than the magmatic activity of other ore field(124–148 Ma) in the Middle-Lower Yangtze River Valley metallogenic belt. It is suggested that the tectonic-magmatic-thermal events in the Ningzhen area is formed under regional lithospheric extension environment, which is also consistent with the tectonic background of the third period of large scale mineralization in South China. The zircon U-Pb ages of the intrusions and the Re-Os ages of molybdenites from the porphyry deposits in the study area demonstrate that the Ningzhen district underwent intensive magmatism and hydrothermal mineralization during the period from 102.5 to 108.0 Ma, which is consistent with the third pulse of large scale mineralization in the South China.
【Fund】: 中国地质调查局长江中下游成矿带地质矿产调查项目(编号:资[2010]矿评01-16-17、[2011]02-18-10、[2012]02-014-013)资助
【CateGory Index】: P597;P611
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