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《Acta Petrologica Et Mineralogica》 2006-06
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Geochemical characteristics and genesis of Zhoukoudian complex

ZHANG Li_fen~1 , ZENG Xia_sheng~2 and ZHANG Shu_ming~ 3,4 (1. Institute of Seismology, CEA, Wuhan 430071, China; 2. Investigating and Foundation Engineering Co. Ltd. in Middle South, Wuhan 430081, China; 3. East China Institute of Technology, Fuzhou 344000, China; 4. China University of Geosciences, Wuhan, 430074, China)  
Based on geochemical characteristics and tectonic setting of intrusive rocks in Zhoukoudian complex and a comparison with adakites, the authors have revealed that these intrusive rocks are similar to adakites in petrological and geochemical characteristics. ~ 143 Nd/~ 144 Nd-~ 87 Sr/~ 86 Sr diagram shows that the projections are in the EMⅠ_rich mantle region, suggesting that their material sources are related to EMⅠ_rich mantle. Besides,εNd(t)-I_ Sr figure proves that the projections are within granulites and pyroxenite xenoliths in Hannuoba basalts. Further research indicates that Zhoukoudian complex was formed by partial melting of young lower crust in the North China craton in Mesozoic.
【Fund】: 国家自然科学基金重点资助项目(40133020)
【CateGory Index】: P584
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