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《Geological Review》 2006-02
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Current Study of ~(210)Pb and ~(137)Cs Geochronology in the Circum-Bohai Sea Region

WANG Fu 1,2),WANG Hong 1,2),LI Jianfen 1),PEI Yandong 1),FAN Changfu 1,2),SHANG Zhiwen 1,2) 1) Tianjin Institute of Geology and Mineral Resources,China Geological Survey,Tianjin, 300170 2) College of Earth Sciences,Jilin University,Changchun,Jilin, 130026  
As an important factor, modern accumulation rates have a significant influence on the recent and present geo-environmental changes in the Circum-Bohai Sea (CBS) region. 210Pb_ exc and/or 137Cs geo-chronological sections at 84 sites ( 210Pbexc sections at 52 sites, 210Pb_ exc and 137Cs sections at 32 sites), determining the modern accumulation rates in the CBS region, were collected. 39 cores are located in sea area and the others located on the coastal lowland and the intertidal flat. 210Pb_ exc and 137Cs sections collected show three essential vertical distribution patterns, (1) Ideal-Decaying-type, (2) Wiggling with Approximate Equivalent Amplitude, and (3) Episodic-Event-Influencing-type. Low accumulation rates of the coastal lowland, high accumulation rates of the intertidal flats and low accumulation rates in the sea areas were identified based on the existing differential accumulation rates. In a ‘high—low—high’ pattern from the Jiyunhe Estuary in north to the Laolangtuozi upper part of the intertidal marsh in south along the western coast of the Bohai Bay, the rate decreases from the Jinzhou Bay intertidal flat to the Liaohe estuary in Liaodong Bay, and episodic high accumulation occurs the Yellow River Delta and the surrounding sea area while high accumulation rates exist in the Laizhou Bay.
【Fund】: 中国地质调查局国土资源调查项目(编号19991300013015)的成果。
【CateGory Index】: P597.3
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