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- W2376627607 abstract "The mantle peridotite xenoliths entrained in the Quaternary alkali basalts in the Aershan--Chaihe area of Inner Mongolia are composed of spinel lherzolite and spinel harzburgite which is slightly higher than the former in quantity. We studied the partial melting process and metasomatism with LA--ICP--MS based on the CPX and Ol analysis in mantle peridotite,combined with the petrographical and geochemical characteristics of peridotite inclusions. The result shows that melting degree of most samples ranges from 10% to 20%,with a few exceptions less than 5%,which implies a depleted mantle source and it was overlapped by silicate melt metasomatic alteration. By comparison with SCLM( sub--continental lithospheric mantle) of the North China Craton,we deduce that it retains appreciable quantity of old mantle residual with little metasomatism in the studied area." @default.
- W2376627607 created "2016-06-24" @default.
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- W2376627607 date "2014-01-01" @default.
- W2376627607 modified "2023-09-23" @default.
- W2376627607 title "Study on SCLM in Aershan--Chaihe area of Inner Mongolia: evidence from trace elements of clinopyroxene" @default.
- W2376627607 hasPublicationYear "2014" @default.
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