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《Earth Science Frontiers》 2003-04
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ON THE SPACE-TIME DISTRIBUTION AND GEODYNAMIC ENVIRONMENTS OF ADAKITES IN CHINA ANNEX: CONTROVERSIES OVER DIFFERING OPINIONS FOR ADAKITES IN CHINA

ZHANG Qi, WANG Yan, LIU Hongtao, WANG Yuanlong, LI Zhitong Institute of Geology and Geophysics , Chinese Academy of Sciences , Beijing 100029, China; Department of Earth Sciences , The University of Hong Kong, Hong Kong , Ch ina; Shenyang Institute of Geological and Mineral Resources, Shenyang 110032, China  
Adakites occur widely in most area of China except for Guangdong, Guangxi, Hunan and Guizhou Provinces, and concentrate mainly on the Paleo-Asian erogenic belt, east of Jinlin and Hei-longjiang and east China, as well as on the Qin-Qi-Kun orogenic belt, Neo-Tethyan erogenic belt and Tibet Plateau, but sporadically in south China. The oldest adakite (about 1 000 Ma) in China occurs associated with ophiolite in NE Jiangxi, while the youngest adakite (60-10 Ma) in China is the Tertiary adakite in Tibet Plateau. All the adakites in China can be divided into two groups: one is Otype adakite, the other is C-type adakite, which are formed by plate subduction and crust thickening, respectively. It is also discussed in the paper that the events of subduction and continental crust thickening in different geological ages and their geodynamic implications which are indexed by the adakites.
【Fund】: 国家“973”项目(G1999043206-05);; 中国科学院知识创新工程项目(KZCX1-07) KZCX2-104
【CateGory Index】: P588.1
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