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《GEOLOGY OF ANHUI》 1994-Z1
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REVIEW ON THE FORMATION, EVOLUTION AND CLOSURE OF THE JINING-CALEDONIAN SEA BASIN IN THE EASTERN PART OF SOUTH CHINA

Yu Dagan(East China Geological Institute)  
The Jinning-Caledonian sea basin in the eastern part of South China was formed in the Qingbeikou periedand experienced three stages of Jinning,early and late Caledonian perieds. The basement of the sea basin was continentalcrust formed in a stretching rift environment. The closure of the sea basin mainly underwent intracontinental underthrustand splice, and was of multistage characters. The high calorific value of the beement of sca basin,especinlly the basementof the Huaxia block,led to the formation of two types of sea basins in the Caledonian,the Xianggui(Hunan andGuizhou)and Ganminyue (Jiangxi,Fujian and Guangdong) sea basins.The basement of the latter is evident in activity,lying over the basement of the Huaxia block , in which there are several intracontinental dynamo-hydrothermal metamor-phic zones.
【CateGory Index】: P54
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