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《Earth Science Frontiers》 2006-02
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Peridotite-melt interaction:an important mechanism for the compositional transformation of lithospheric mantle

ZHANG Hong-fuState Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China  
Peridotite-melt/magma interaction has usually been used to interpret the petrogenesis for those rocks that have disequilibrated textures and mineral compositions,which range from ophiolitic peridotites, orogenic peridotites, ultra-mafic intrusive complexes, to mantle xenoliths. There are two major types of peridotite-melt reaction: i.e. dissolution of olivine (and clinopyroxene) and precipitation of orthopyroxene, or dissolution of orthopyroxene and precipitation of olivine (and clinopyroxene). The result of the reaction leads not only to a change in mineral percentages, but also to a change in mineral compositions;the latter has not been paid enough attention. The discovery of zoned mantle olivine and pyroxene xenocrysts, especially zoned mantle peridotitic xenoliths in Mesozoic basaltic rocks from eastern North China, indicates that peridotite-melt interaction was widespread in Mesozoic lithospheric mantle beneath the southeastern North China craton. Such interaction could be an important mechanism for the compositional transformation and rapid enrichment of the lithospheric mantle. This is the first case in the world for large-scale compositional changes of the lithospheric mantle resulting from peridotite-melt interaction. The reactant melts were mainly derived from two sources: crustal materials and/or asthenosphere. Reaction of peridotites with melts from different sources results in different compositional changes.
【Fund】: 国家自然科学基金委员会杰出青年科学基金项目(40225009);; 国家自然科学基金委员会大陆动力学重点项目(40534022)
【CateGory Index】: P588.12
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