The mapping of geochemical provinces in China based on Pb isotopes

被引:110
作者
Zhu, BQ
机构
[1] Academia Sinica, Guangzhou, China
基金
中国国家自然科学基金;
关键词
D O I
10.1016/0375-6742(95)00011-9
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The comparison of Pb isotopic compositions for Various ores and rocks has revealed that the lateral variation between different terranes is greater than the vertical variation between crust and mantle, which is useful for geochemical mapping. Based on a three dimensional topological diagram of ph isotopes, six geochemical provinces can be recognized in China, namely southern China, Yangtze, northern China, northern Xinjiang, Jiamusi and Tibet. The application of Pb isotopes to regional mapping provides important background data for geochemical prospecting as it establishes the tectonic boundaries of terranes and identifies the source regions of mineralization, magmatism and sedimentation. It also provides information on the origin of pollution and cultural relies.
引用
收藏
页码:171 / 181
页数:11
相关论文
共 48 条
[1]   TOPOLOGY IN ISOTOPIC MULTISPACE AND ORIGIN OF MANTLE CHEMICAL HETEROGENEITIES [J].
ALLEGRE, CJ ;
HAMELIN, B ;
PROVOST, A ;
DUPRE, B .
EARTH AND PLANETARY SCIENCE LETTERS, 1987, 81 (04) :319-337
[2]   MAJOR ELEMENT, REE, AND PB, ND AND SR ISOTOPIC GEOCHEMISTRY OF CENOZOIC VOLCANIC-ROCKS OF EASTERN CHINA - IMPLICATIONS FOR THEIR ORIGIN FROM SUBOCEANIC-TYPE MANTLE RESERVOIRS [J].
BASU, AR ;
WANG, JW ;
HUANG, WK ;
XIE, GH ;
TATSUMOTO, M .
EARTH AND PLANETARY SCIENCE LETTERS, 1991, 105 (1-3) :149-169
[3]  
CHEN BM, 1984, J STRUCT CHEM, V3, P37
[4]  
CHEN DG, 1990, UPPER MANTLE FEATURE, P124
[5]  
CHEN HS, 1987, GUANGXI GEOL ACTA, V1, P46
[6]  
Chen JF, 1992, STUDIES STRUCTURE EV, P119
[7]  
CHEN YW, 1991, P OCEAN ENV AREA NAN, P243
[8]  
Chen YW, 1980, GEOCHEMISTRY-USSR, V3, P215
[9]  
Deng F.L., 1987, GEOCHIMICA, V2, P141
[10]  
DePaolo D.J., 1981, J GEOPHYS RES, V86, P407