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《Journal of Jiling University (Earth Science Edition)》 1989-02
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ORIGIN OF THE SPILE-QUARTZ KERATOPHYRE SERISE,BAIYIN DISTRICT, GANSU PROVINCE, CHINA

Jiang Xinming Cong Guixin(Academy of Geology,Ministry of Metallurgical Industry,Tianjin)  
The spilite-quartz keratophyre series in Baiyin district was formed on island arc or in back-arc basin related to convergence plate tectonics that gave birth to the tholeiitic magma and provided the source of sodium for promoting Na-metaso-mation.The latter process holding in spilite-quartz keratophyre started while it was in the magma chamber and continued in its ascension and spreading over the sea floor. Thus, both textures of primary magmatic rocks and alkali metasomatism might be discovered in the spilite-quartz keratophyre rocks though its origin should be attributed to metasomatism.
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