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《地球科学》 1989-04
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FEATURES AND EMPLACEMENT OF THE ZHOUKQUDIAN STOCK, BEIJING

Wang Renjing Ma Changqian ( China University of Geosciences, Wuhan 430074 )  
The Zhoukoudian granitoid stock in western Beijing is a concentric complex which was formed by repeated pulsative intrusions. The first intrusion is finegrained quartz diorite which scattered in the margin,and the second is granodio-rite which is the main part of the pluton. From the center to the margin, the latter is again divided into three gradually transitional concentric phase zones. Chemical analyses of the rocks indicate that SiO2 increases very quickly, and Na2O and K2O rise slowly, while MgO, FeO, Fe2O3, CaO and A12O3 decrease from the early intrusive body through the margin of the late intrusion to the center. Petrochemical and mineralogical features indicate that it is I-type granitoid rock. Structure features of the pluton and aureole rocks show that the emplacement of the stock was a diapiric process.
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