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《Geochimica》 2002-03
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Constraints on the Cenozoic tectonic evolution of northern South China Sea (I): Mantle derived xenoliths

XU Yi gang1,3, HUANG Xiao long1, YAN Wen2, LIU Ying1, CHEN Xiao ming3(1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China; 2. South China Sea Institute of Oceanography, Guangzhou 510300, China; 3. Department of  
The mantle heterogeneity and complex mantle processes are revealed on the basis of studies of mantle derived xenoliths in Cenozoic basalts in thenorthern South China Sea. Clinopyroxenes (Cpx) in some peridotites display extremely low Ti contents ( 160 μg/g) inconsistent with their relatively high Cpxmodes (8%~12%). Peculiar major element compositions and fractionated HREEin Cpx requires a polybaric melting to take place in the mantle beneath south China. These patterns can be modeled as residues of 23%fractional melting froma primitive mantle, first in garnet stability field then continuing in spinel stability field after breakdown of garnet to pyroxenes and spinel. These residueshave been further metasomatized by silicate melts and aqueous fluids. The traceelement characteristic of the peridotite xenoliths suggests a rift type mantle under this region, which is significantly different form those above the subduction zone or those affected by subduction related processes. The negative correlation between Fo in olivine and equilibration temperature suggests a stratified mantle beneath South China. The lower part of the upper mantle predominantly consists of fertile and moderately depleted peridotites which plot within the Phanerozoic mantle domain. In contrast, the upper layer contains harzburgite and Cpx poor lherzolite that are strongly affected by metasomatism of melt/fluid ofhighly variable compositions. The anomalously high orthopyroxene mode (up to 47%) rends some of these refractory samples compositionally similar to the Proterozoic/Archean mantle. Such lithosphere architecture may have resulted from partial replacement of the Archean Proterozoic lithosphere by the asthenosphere that rose adiabatically subsequent to lithospheric thinning during the Cenozoic. The xenolith data support the contention that the formation of South China Sea isrelated to southward migration of lithosphere extension, rather than passive back arc basin.
【Fund】: 国家杰出青年基金(49925308);; 中国科学院知识创新工程重要方向项目(KZCX2-209);; 国家攀登项目(95-预选-39)
【CateGory Index】: P594
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