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《Geological Science and Technology Information》 2001-03
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DISCUSSION ON THE METALLOGENIC EPOCH OF GOLD DEPOSITS IN SOUTH CHINA:A CONCURRENT DISCUSSION ON THE PAPER OF WANG XIUZHANG ET AL'S "MAIN CHARACTERISTICS OF CALEDONIAN GOLD DEPOSITS IN SOUTH CHINA

Chen Bailin (Institute of Geomechanics,CAGS,Beijing 100081,China)  
South China has presently become one of the most important gold producing areas.It is geologically either a part of paleo Tethys metallogenic province or controlled by strong intraplate deformatino in East China and circum Pacific metallogenic belt in Mesozoic era.The gold deposits in South China featured by closely relating to the metamorphic rocks,mainly from metamorphic rocks for metallogenic materials,strongly controlled by tectonic zone,magmatic activities and ductile shear zone.The metallogenic epoch of gold deposits the area can be summarized as follows.① There is one older epoch (Proterozoic era) and one younger epoch (Mesozoic era).②The age of metallogenic material is much older than the age of the deposits.③Mesozoic era is the most important metallogenic epoch of gold deposits and ④ there is a difference of metallogenic epoch among in the south and the north and the northwest parts of China.Moreover,the author points out that structural deformation may cause the loss of radioactive isotope in minerals and rocks which affect the accuracy of the isotope age.
【CateGory Index】: P618.51
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