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《Chinese Journal of Geophysics》 2013-08
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Magnetic properties of minerals recorded by the borehole WJ and Late Quaternary transgressions in the Taihu plain,southern Yangtze Delta

CHEN Ting1,2,3,WANG Zhang-Hua4*,QIANG Xiao-Ke1,MA Chun-Yan3,ZHAN Qing3 1 State Key Laboratory of Loess and Quaternary Geology,Institute of Earth Environment,Chinese Academy of Sciences, Xi′an 710075,China 2 University of Chinese Academy of Sciences,Beijing 100049,China 3 Department of Geography,East China Normal University,Shanghai 200062,China 4 State Key Laboratory for Estuarine and Coastal Research,East China Normal University,Shanghai 200062,China  
Based on paleomagnetism and AMS14C ages,we reconstructed the evolution of sedimentary environment and transgression events during the Late Quaternary by examining the lithology,magnetic properties,grain sizes,and foraminifera of sediments from a borehole named WJ in the Taihu plain,southern Yangtze Delta,China.We also examined the applications of magnetic proxies to distinguishing depositional environments in the estuary-delta area.The results show that the sediment sequence of the WJ borehole can be divided into four periods,i.e.Mid-Pleistocene stage I,Mid-Pleistocene stage II,Late-Pleistocene,and Holocene.Their depositional geomorphological conditions were fluvial-lacustrine,coastal-terrace,mouth bar-estuary-tidal flat-terrace,and lacustrine plain,respectively.Three transgression events were detected in the borehole WJ,which happened during the late Mid-Pleistocene,MIS5 and MIS3 of Late-Pleistocene.Among them,the MIS5e transgression was the strongest one.Additionally,the transgression was intensified significantly in late MIS3.Magnetic properties were strongest for the tidal flat and mouth bar sediments with notably high values of χlf,SIRM and HIRM.
【Fund】: 国家自然科学基金项目(41176070);; 河口海岸学国家重点实验室科研业务费(2010RCDW05)资助
【CateGory Index】: P318.4
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