浙江花岗岩中斜长石钾交代产生的条纹长石(英文)  

K-METASOMATISM OF PLAGIOCLASE TO PRODUCE PERTHITE IN GRANITIC ROCKS OF ZHEJIANG PROVINCE,SOUTHEAST CHINA

作　　者：Moustafa El Omella 巩恩普[1] 孙旭东[1] Abdalghni Saleh 

机构地区：[1]东北大学,辽宁沈阳110004

出　　处：《地质与资源》2003年第3期129-138,共10页Geology and Resources

基　　金：ThisstudywassupportedbytheChinaScholarshipCouncil(GrantNo.160),NationalNatureScienceFoundationofChina(GrantNo.400722006)andtheKeyTaskProjectofScienceandTechnologyofLiaoningProvince(GrantNo.2001230001)

摘　　要：对研究区内花岗岩类的60个薄片进行了岩相学研究.研究的目的是确定区内岩石中普遍存在的矿物组成及结构类型. 碱性长石花岗岩为中粒,块状,白到粉色,主要由碱性长石和石英组成,含镁铁质矿物如黑云母、白云母等,含副矿物磷灰石、褐帘石和锆石.碱性长石占岩石组成的绝大部分,包括微斜长石和微条纹长石.斜长石晶体一般具钠长石—卡斯巴双晶,无条带. 正常花岗岩通常比碱性长石花岗岩稍暗,中—粗粒,一般为半自形粒状或花岗结构.长石和镁铁质矿物都以半自形晶体出现,而石英则通常为灰色玻璃质,充填于其他矿物颗粒之间. 对碱性斜长花岗岩和正常花岗岩所做的化学分析显示,这些过铝质岩石呈高Si、Al、Na和K含量的特征.其中碱性斜长花岗岩的氧化物含量为:SiO2 76.61%,TiO20.15%,Al2O3 12.81%,Fe2O3 0.67%,FeO0.5%,MnO0.01%,MgO0.19%,CaO0.18%,Na2O3.82%,K2O4.46%,P2O5 0.01%.正常花岗岩中氧化物含量为:SiO2 73.76%,TiO2 0.12%,Al2O3 13.93%,Fe2O3 0.77,FeO0.58%,MnO0.03%,MgO0.16%,CaO0.31%,Na2O3.04%,K2O3.64%,P2O5 0.02%. 关于花岗岩类中钾长石的成因有2种观点.一种认为形成于岩浆的结晶作用,钾长石或是缓慢长大,或是在成核作用后快速长大;另一种观点则认为钾长石是钾交代成因的.岩浆成?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.

关 键 词：花岗岩 岩相学 矿物组成 碱性长石 石英 

分 类 号：P586[天文地球—岩石学]