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《Geology-geochemistry》 2002-02
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A DISCUSSION ON THE METALLOGENIC EPOCH OF GOLD DEPOSITS IN CHINA

Chen Bailin (Institute of Geomechanics, Chinese Academy of Geological Sciences,Beijing 100081)  
The metallogenic epoch of gold deposits in China can be summarized as "one older epoch and one younger epoch, different between the east and the west and between the south and the north of China". The older gold metallogenic epoch from Neo Archean era to Paleo Mid Proterozoic (2 600~1 400 Ma), and the younger metallogenic epoch is mainly in the Mesozoic era and partly in the Upper Paleozoic era (300~100Ma). The older gold metallogenic epoch ranges from Neo Archean to Paleo Proterozoic (2 600~1 800 Ma) in North China, but Mid Proterozoic (1 800~1 400 Ma) in South China, while the younger metallogenic epoch is from Yanshanian (140~100Ma) in North China (e.g. Jiaodong area) to Indo Chinese (230~190Ma) in South China (Hainan, West Guangdong, and part of Fujian ). Similarly, Mid Proterozoic (140~100Ma) is the most important metallogenic epoch in East China, but Upper Paleozoic (300~230Ma) is only in West China (Beishan, Tianshan and North Xinjiang are the typical areas). Meanwhile, gold deposits in China have some other features: (1) the age of metallogenic material is much older than the age of the deposit; (2) multi periodic superimposed metallogenesis is very common; and (3) gold deposits of the magmatic hydrothermal type are the most important in China. All above is controlled by the distinctive geotectonic framework and evolutionary history of China.
【Fund】: 新一轮国土资源大调查项目 (K1.1.2 .3 K1.2 .4.4) ;; 原地质矿产部定向研究基金 (地科定 96 2 1)
【CateGory Index】: P618.51
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