陆壳深部结构研究的地质地球化学方法及其在华南地区的应用  

THE GEOLOGICAL-GEOCHEMICAL METHOD IN THE STUDY OF THE DEEP STRUCTURE OF CONTINENTAL CRUST AND ITS APPLICATION IN SOUTH CHINA

作　　者：金文山[1] 赵风清[1] 甘晓春[1] 王祖伟[1] 

机构地区：[1]天津地质矿产研究所

出　　处：《安徽地质》1994年第Z1期122-134,共13页Geology of Anhui

基　　金：地质矿产部"华南大陆深部地壳结构及演化"研究项目资助

摘　　要：应用地质地球化学方法研究华南陆壳深部结构表明：华南存在一个广泛的统一的早前寒武纪（早元古代至晚太古代）的结晶基底，华南下陆壳的平均组分相当于中酸性，其中扬子地块下陆壳的成熟度比华夏地块的低。The study result of deep structure of the continental crust by applying the geology-geochemistry methodin South China shows that there exists a broad and integratal crystal basement of the early Precambrian(Early Proterozoicto late Archean), and the average composition of the lower continental crust of South China is equivalent to medium- acid rocks,and the maturity of the lower continental crust of “Yangtze massif”is lower than that of “Cathaysia massif”.

关 键 词：陆壳深部结构 地质地球化学方法 华南 

分 类 号：P59[天文地球—地球化学]