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《Journal of Changchun University of Science and Technology》 2001-04
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TEMPORAL-SPATIAL EVOLUTION OF GRANITOID-HOSTED GOLD DEPOSITS IN EASTERN PART OF NORTH CHINA PLATFORM

LIANG Hua_ying, WANG Xiu_zhang, CHENG Jing_ping (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640,China)  
Many granotoid-hosted gold deposits are distributed in eastern part of North China Platform. They can be divided into synintrusive body and postintrusive body types. The former occurs in the border area of Hebei and Liaoning provinces with near formative time (mainly during Middle Jurassic period)of magmatic body and gold mineralization. The latter mainly appears in Liaoning and Shandong Provinces with older age of magmatic body (mainly during Jurassic period) and with younger time (minly during Cretaceous period)of mineralization. The time differences are larger than 20~120 Ma. Gold mineralization getting younger southeast-eastern wards shows that subduction of Pasific Plate under Asia Plate played an important role in tectonic-magmatic activition of North China Platform and formation of related gold deposits. Part of mineralization getting younger northwards indicates the influence of collison of Siberia Plate with Asia Plate on the formation of gold deposits in the area.
【Fund】: 国家自然科学基金资助项目 ( 4 9772 114 ;;4 93 72 10 5 )
【CateGory Index】: P618.51
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