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《GEOCHIMICA》 1995-01
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GEOCHEMISTRY OF CENOZOIC BASALTS FROM EASTERN CHINA──Ⅰ.MAJOR ELEMENT AND TRACE ELEMENT COMPOSITIONS:PETROGENESIS AND CHARACTE-RISTICS OF MANTLE SOURCE

Liu Congqiang(Institute of Geochemistry, The Chinese Academy of Sciences, Guiyang 550002)Xie Guanghong(Guangzhou institute oj Geochemistry, The Chinese Academy ot Science,, Guangzhou 510640)Akimasa Masuda(Department of Chemistry, University of Electronic-  
Cenozoic basalts from eastern China including tholeiitic, alkalic, picritetrachy and potassic basalts were studied in this paper. The variation of both major element and trace element abundances shows that these Cenozoic basalts were derived from the partial melting of mantle at various depths and subsequent fractional crystallization. Variable ratios of highly imcompatible elements might be related to lithospheric mantle metasomatism. It appears that the upwelling of asthenospheric magma and the melting of overlying heterogeneous mantle lithosphere generate the Cenozoic basalts of eastern China.
【CateGory Index】: P588.1
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