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《Journal of Jiling University (Earth Science Edition)》 2004-03
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Charateristics and genesis of the intermediate and intermediate- basic volcanics in Pinggang-Weijin area, Jilin Province

XIE Yi-hong~(1), HU Shuang-huai~2,LU Feng-xiang~(3), ZHU Qin-wen~(3) (1. Shenzhen College of Techniques and Profession, Shenzhen518049, China; 2.Shenzhen Geotechnical Investigation and Surveying Institute, Shenzhen518028,China; 3.China University of Geosciences, Wuhan430074, China)  
The petrologic characteristics of the intermediate and intermediate-basic volcanics from Pinggang-Weijin area are: main rocks are shoshonite, basalt-andesite, andesite and latite; magmatic evolution series belongs to high potassium calc-alkali series, accompanied by minor shoshonitic series and tholeiitic series; rich in LREE and lack in Eu anomaly; Sr、K、Rb、Ba、Th enriched, but Nb is lower, indicating the volcanic rocks in the area were formed in a mixed tectonic setting of both volcanic arc and inter-plate. Mg and Ni contents in shoshonite indicate that the shoshonite was derived from an evolved basic magma. Based on Sr/Nd ratios and crystalline depth of pyroxene megacrystals in dacite and crust thickness of the east side of the Songliao Basin, it is inferred that the shoshonitic magma originated from primary magm from the mantle. It is recognized that the formation of shoshonite is related to the density of magma and plagioclase and to the crystallizing pressure of plagioclase based on estimation on the density of magma, crystalline pressure and temperature.
【Fund】: 教育部博士点基金项目资助(9549110)
【CateGory Index】: P588.1
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