Conclusions
The oxygen isotopic composition of mantle-derived materials from Anhui-Jiangsu basalt province indicates the mantle heterogeneity in δ18O and the coherence between δ18O and Sr-Nd isotopic composition for the mantle beneath the province. The oxygen isotopic compositions of the basalts from the Luhe-Yizheng area, the clino- and orthopyroxenes in spinel lherzolite xenoliths from the province and mineral megacrystals from Nushan and Panshishan are as same as those of normal mantle in a first approximation. The basalts from the Jiashan-Lai’an area have high δ18O, and Nd-Sr isotopic compositions of the basalts are the same as those of EM-type enriched mantle. The residual of recycled crustal materials supply the relevant enriched component, and mantle mixture produces the enriched source from which the basalts were derived.
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Zhi, X., Li, Y. & Zheng, Y. Oxygen isotope composition of mantle-derived materials from Anhui-Jiangsu basalt province, East China. Chin.Sci.Bull. 42, 662–665 (1997). https://doi.org/10.1007/BF03182646
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DOI: https://doi.org/10.1007/BF03182646