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《成都地质学院学报》 1987-03
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GEOCHEMISTRY OF THE LATE PERMIAN EMEISHAN BASALTS AND IMPLICATION OF SUBCOTINENTAL MANTLE EVOLUTION

Wang yunliang Xiong Shunhua S.S.Hughes~① Li Juchu Li Jianlin Tong Chunhan Zhou Rongsheng ①Permanent Address:The Radiation Center Oregon State University Corvallis, Oregon 97331, USA  
Emeishan basalts were sampled from Emei, Tangfang and Ertan sections. Multi-element chemistries indicate a predominance of low-MgO in the Emei and Tangfang sections, while the Ertan suite is of high-Mgo variety, Consanguinity among all the three suites is suggested by consistently high TiO_2,K_2O, incompatible trace element abundances, and fractionated rare earth element patterns. Isotopic data for Emei samples ~(37)Sr/~(86)Sr=0.7066-0.7082, Rb/Sr=0.02-0.12, ~(143)Nd/~(144)Nd=0.51171-0.51174. The primary magmas of all three groups can be modeled using a uniformly metasomatized mantle source.Trace element models allow the derivation of Emei and Tangfang primary magmas by 10—15 percent partial melting from spinel lherzolite,Ertan primary alkali olivine basalts are derived by 7—10 percent partial melting of the same source.A mechanism of mantle enrichment is proposed which requires the metasomatic stabilization of phlogopite which is depleted during partial melting.
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