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《Geochimica》 1998-06
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A PALAEOPROTEROZOIC A-TYPE RHYOLITE

Yu Jinhai; Wang Dezi; Geng Jianhua (Department of Earth Sciences,Nanjing University, 210093)  
The rhyolites in the Upper Luliang Group of Shanxi Province of China are Palaeoproterozoic A-type volcanic rocks. They are characterized by high SiO2, Na2O +K2O, Zr, Nb, Ga, Y and REE contents and large FeO* / MgO, Rb / Sr and Ga / Al ratios, and low CaO, Sr and Eu contents, and formed in the rifting setting of continental margin. Their chemical features and isotopic data (high εNd(t) and low Sr initial ratios) suggest that original granitic magma derived from the partial melting of Late Archean lower crust metamorphic rocks due to the influence of basaltic magma and hot fluid in the rifting. A-type rhyolites formed after the fractional crystallization of the dominant feldspar.
【Fund】: 国家自然科学基金!49202024
【CateGory Index】: P588.14/P5
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