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《GEOLOGY-GEOCHEMISTRY》 1997-04
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GENETIC MECHANISM OF PLAGIOCLASE ZONING

Wu Pingxiao Wu Jingpind Xiao Wending Li Caiwei (Guangzhou Institute of Corhemistry. Chinese Academy of Sciences, Guangzhou, 510640) (Department of Applied Chemistry, China Universty of Geosciences, Wuhan, 430074)  
This paper systematically ana1yses the current situation of research on plagioclase zoning and points and that the middle- and small-scale oscillatory zoning in plagioclase is formed organization. It has nothing to do with environmental factors. The large-scale oscillatory zoning in plagioclase is formed as a result of the "periodic" vibration of environment (temperature, pressure), but not of self-organization. Its formation has recorded the magmatic activities (temperature, pressure and concentration of magma). The small-scale oscillatory zoning in plagioclase is formed at the crystal-growth temperature near the solidus. When the crystallization temperature is blow the solidus, non-oscillatory zoning or dendritic crystal and glass mass will be formed. The nonoscillatory zoning in plagioclase is formed as a result of persisting variations in temperature or pressure of the environment. Its crystallization temperature is lower than that of the small-scale zoning within the large-scale zoning, or its nonequilibrium is greater.
【CateGory Index】: P571
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