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《Geochimica》 2005-05
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Abundances of chemical elements in granitoids of China and their characteristics

SHI Chang-yi, YAN Ming-cai, LIU Chong-min, CHI Qing-hua, HU Shu-qi, GU Tie-xin, BU Wei, YAN Wei-dong (Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geol ogical Sciences, Langfang 065000, China)  
About 6 080 samples were collected mainly from about 750 large to mi ddle representative granitoid bodies in whole China and they were combined into 768 composited samples for being analyzed in the laboratories. All the samples w ere processed and prepared by the contamination-free preparing scheme. About 70 elements of Ag, As, Au, B, Ba, Be, Bi, Cd, Cl, Co, Cr, Cs, Cu, F, Ga, Ge, Hf, H g, In, Li, Mn, Mo, Nb, Ni, P, Pb, Rb, S, Sb, Sc, Se, Sn, Sr, Ta, Th, Ti, Tl, U, V, W, Zn, Zr, SiO2, TiO2, Al2O3, Fe2O3, FeO, MnO, MgO, CaO, Na2O, K2O, P2O5, H2O +, CO2, Ce, Dy, Er, Eu, Gd, Ho, La, Lu, Nd, Pr, Sm, Tb, Tm, Y and Yb were analy zed with multiple advanced reliable analytical methods relying mainly on ICP-MS , INAA and XRF. National preliminary geochemical certified reference materials s uch as GSR-1, GSR-2, GSR-4, GSR-5, GSR-14, GSS-9, GSD-9, GSD-1a, GAu-10 , GAu-11, Au-2, GAu-8, GAu-9 and duplicates were used to monitor rigidly the analysis quality in order to ensure the accuracy and reliability of analytical data. Based on the actual analytical data, the total average chemical compositio ns and element abundances of about 67 chemical elements of SiO2, Al2O3, Fe2O3, F eO, MgO, CaO, Na2O, K2O, H2O+, CO2, TFe2O3, Ag, As, Au, B, Ba, Be, Bi, Cd, Cl, Co, Cr, Cs, Cu, F, Ga, Ge, Hf, Hg, Li, Mn, Mo, Nb, Ni, P, Pb, Rb, S, Sb, Sc, Se, Sn, Sr, Ta, Th, Ti, Tl, U, V, W, Zn, Zr, La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho , Er, Tm, Yb, Lu and Y in China's granitoids, granitoids in different geotectoni c units and different geological ages are calculated and presented in this paper . It is sufficiently discussed on the distribution patterns of petrochemical par ameters, trace element contents and rare earth element distributions of the gran itoids. δvalue of Chinas granitoids is 2.12,K/Na=1.22,A/CNK=1.1,C/ACF=0.13 , ∑REE=168, LREE=133.2, HREE=15, LREE/HREE=8.91, (La/Yb)N=9.34,δEu=0.597. Dist ribution patterns of element abundances in the granitoids of different geologica l ages are different. They have different features. Element abundances of the gr anitoids in different geotectonic units are very difference. Different geotecton ic units have different features of element abundances. It shows that element ab undance has some regional features.
【Fund】: 科技部社会公益研究专项项目(2001DIB10076)~~
【CateGory Index】: P588.121
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Chinese Journal Full-text Database 10 Hits
1 Hou Wei Chen Huifang Liang Xinquan Wang Kefu(Changsha Institute of Geote ctonics, Academia Sinica);THE ESTABLISHMENT OF PRECA MBRIAN STRATA AND NEW RECOGNITION OF THE GEOTECTONIC EVOLUTION IN HAINAN ISLAND[J];;1992-02
2 ZOU Heping (Changsha Institute of Geotectonics, A cademia Sinica, Changsha, 410013);ON THE PROBLEM ABOUT THE CRUST'S ATTRIBUTION OF SOUTH CHINA SEA BASIN——DISCUSSION FROM COMPARATIVE STUDY ON BASALTS OF SEAMOUNTS IN SOUTH CHINA SEA BASIN AND THE NEIGHBORING AREAS[J];Geotectonica Et Metallogenia;1993-04
3 DING Shijiang (Hainan Exploration Institute of Geosciences, Haikou 570005);THE GEOLOGICAL CHARACTERISTICS OF GEZHEN INTRUSIVE MASS IN WESTERN HAINAN AND ITS SIGNIFICANCE[J];Geotectonica Et Metallogenia;1995-04
4 TANG Hong-feng(Open Laboratory of Ore Deposit Deochemistrp Institute of Geochmistry Academia Sinica, Guiyang 550002, China);GEOCHEMICAL CHARACTERISTICS OF THE BASALT FROM CHENXING, HAINAN ISLAND,AND THEIR TECTONIC IMPLICATION[J];GEOTECTONICA ET METALLOGENIA;1999-04
5 XU De-ru(Changsha Institute of Geotectonics, Academia Sinica, Changsha 410013, China);A STUDY ON THE ROCK CHEMISTRY OF LAMPROPHYRE IN THE GEZHEN GOLD-BEARING ZONE, HAINAN ISLAND[J];GEOTECTONICA ET METALLOGENIA;1999-04
6 Wu Qinsheng Xu Junzhen Yang Zhi (Institute of Geology, Ministry of Metallurgical Industry);Sr ISOTOPIC CHARACTERISTICS OF GEJIU Sn-BEARING GRANITES AND A STUDY OF ORESEARCH INDICATORS[J];Geochimica;1984-04
7 Zhu Bingquan Wang Huifen(Institute of Geochemistry, Academia Sinica);Nd-Sr-Pb ISOTOPIC AND CHEMICAL EVIDENCE FOR THE VOLCANISM WITH MORB-OIB SOURCE CHARACTERISTICS IN THE LEIQIONG AREA, CHINA[J];Geochimica;1989-03
8 Yu Shoujun Xia Ping Deng Tieyin Li Qiang(Department of Geology, Zhongshan University, Guangzhou 510275)Chen Yuwei(Institute of Geochemistry, Academia Sinica, Guangzhou 510640);CHARACTERISTICS AND U-Pb ISOTOPIC AGES OF ZIRCONS IN THE MIDDLE PROTEROZOIC GRANITOIDS FROM BAOBAN AREA, HAINAN PROVINCE[J];Geochimica;1992-03
9 QU Xiao-ming;WANG He-man;RAO Bing (Department of Earth Sciences, Nanjing University, Nanjing 210093, China);Partial melting experiments of Jiaodong Group and their implication for the origin of the granites[J];GEOCHIMICA;2000-02
10 XU De ru1,2, LIANG Xin quan2, TANG Hong feng1(1. Changsha Institute of Geotectonics, Chinese Academy of Sciences, Changsha 410013, China; 2. Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China);Geochemical characteristics of Baoban Group metasedimentary rocksin western Hainan, China[J];Geochimica;2002-02
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