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《Oceanologia Et Limnologia Sinica》 2001-03
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QUANTITATIVE PARTITION OF MIXED SURFACE SEDIMENTS FROM THE MIDDLE OKINAWA TROUGH INTO THEIR END-MEMBERS USING Sr-Nd ISOTOPE

MENG Xian Wei, DU De Wen, WU Jin Long  (First Institute of Oceanography, State Oceanic Administration; Key Laboratory of Marine Science and Numerical Modeling, State Oceanic Administration, Qingdao, 266003)  (First Institute of Oceanogr  
Provenance of sediments from the meddle Okinawa Trough has always been a focused problem, for which, many researches have conducted in terms of the mineralogy and geochemistry. However, none of them is not concerned with quantitative partition of mixed sediments according their endmembers. In the present paper, the provenance of mixed surface sediments from the middle Okinawa Trough is discussed using Sr and Nd isotopes, on the basis of which the sediments are partitioned into endmembers using strontium isotope. It is shown that the 87 Sr?/ 86 Sr and 143 Nd?/ 144 Nd ratios of silicate facies in mixed sediments of the western slope from the middle Okinawa Trough are equal to those of silicate facies in the sediments from the East China Sea shelf. 87 Sr?/ 86 Sr and 143 Nd?/ 144 Nd ratios of silicate detritus in the sediments from the bottom and eastern slope of the middle Okinawa Trough are between those from China's land and those of volcanoclastic materials of the Okinawa Trough, demonstrating the nature of two end member mixture. Quantitative partition illustrates that sediments from the bottom and eastern slope of the middle Okinawa Trough are dominated by terrigenous detritus, maximum content accounting for 91 07%. Terrigenous detritus gradually decreased from the west to the east, and minimium content is located on the eastern slope, accounting for 14%. Oppositely, volcanic detritus has a maximium on the eastern slope, accounting for 64.92%; it gradually decreases to zero to wards the west.
【Fund】: 国家自然科学基金!资助项目 ;4 970 60 68号;; 国家自然科学重点基金!资助项目 ;4 973 62 1 0号
【CateGory Index】: P736.2
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