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《Geochimica》 2004-06
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Abundance of mercury in crust,rocks and loose sediments

CHI Qing-hua Applied Geochemistry Research Cent er,Institute of Geophysical and Geo chemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China Correspondence should be addressed to CHI Qing-hua(E-mail:qhchi888@heinfo.net)Received March 25,2004;revised May 17,2004;accepted July 21,2004;published November,2004  
The mercury abundance in crust,rock s and loose sediments is an important parameter in geochemistry.Along with the breakthrough of the an alytical techniques of mercury in 1980s and the accumulation of a huge amount of reliable analytical data o f mercury at present,it is found that it is not suitable now to quote the mercury abundance in crust,rocks and loose s ediments published before 1970s as evaluating criterion.According to the literatures about the mercury conte nts in crust,rocks and loose sedimen ts published in recent twenty years a nd a huge amount of reliable analytical d ata in the study about crust and rocks accumulated,as well as the mercury contents in flood plain sediments in Kazakhstan,Colombia,and Brazil in IGCP 360“Global Geochemical Baseline”project,it is recommended that the mercury abundance in the crust and in t he exposed crust are 7and 13ng /g,the average contents of mercury in rocks,igneous rocks,sedimentary rocks a nd metamorphic rocks are 12.5,6.9,22.6and 8.6ng /g,those in continent al loose sediments,stream sediment s,flood plain sediments,soils and shallow-sea sediments are 60,60,60,65and 25ng /g,respectively.These greatly improve the mercury abun-dance in the crust,rocks and loose se diments,and these have an immense pr actical meaning for theory geochem-istry,exploration geochemistry,e cological geochemistry and environ mental geochemistry.
【Fund】: 国家重点基础研究发展规划项目(1999CB043215);; 原地质矿产部重点基础地质研究项目(8502212)
【CateGory Index】: P618.68
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