Abstract：The perthitic feldspars described in this study are in granites of Zhejiang Province in which the perthite textures appear to have formed as a result of a specific sequences of metasomatic events at the deuteric stage of crystallization and in a chemical environment in which K-metasomatism was enrichment. Perthite textures commonly found in potash feldspars in granitic rocks have generally been attributed to one of two well-established modes of occurrence, either exsolution or replacement process.
作者简介: Moustafa El Omella (1967-),male,Egyptian,M.Sc.of Geology Department,Faculty of Science,Suez Canal University (1997);PhD student of Geology department.Northeast University,China.Contact address:Geology Department,Northeast University,Shenyang 110004,China;Geology Department,Suez Canal University,Ismailia,Egypt.E-mail:elomella@hotmail.com.
引用本文:
Moustafa El Omella, 巩恩普, 孙旭东, Abdalghni Saleh. 浙江花岗岩中斜长石钾交代产生的条纹长石[J]. 地质与资源, 2003, 12(3): 129-138.
Moustafa El Omella, GONG En-pu, SUN Xu-dong, Abdalghni Saleh. K-METASOMATISM OF PLAGIOCLASE TO PRODUCE PERTHITE IN GRANITIC ROCKS OF ZHEJIANG PROVINCE,SOUTHEAST CHINA. GEOLOGY AND RESOURCES, 2003, 12(3): 129-138.
2003, Vol. 12 
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