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HE Zhi-gang, WU Chao-yu, MO Wen-yuan, TANG Zhao-min. A preliminary study on sediment flux in the Zhujiang River Delta during the postglacial period[J]. Haiyang Xuebao, 2006, 28(6): 72-77.
Citation: HE Zhi-gang, WU Chao-yu, MO Wen-yuan, TANG Zhao-min. A preliminary study on sediment flux in the Zhujiang River Delta during the postglacial period[J]. Haiyang Xuebao, 2006, 28(6): 72-77.

A preliminary study on sediment flux in the Zhujiang River Delta during the postglacial period

  • Received Date: 2005-12-29
  • Rev Recd Date: 2006-03-29
  • The sequence boundary and maximum flooding surface of the postglacial transgressive cycle in the Zhujiang River Delt a have been identified by 283 and 269 cores,respectively.On the basis of these data,the sediment amounts of postg lacial,transgressive and regressive periods in the Zhujiang River Delt a have been worked out.The results show that the sediment amounts of post glacial,transgressive and regressive periods are 114.09,36.70 and 77.39 Gt,respectively.The sediment amounts of regressive period are more than those of the transg ressive period.If the annually averaged silting sediments around the river mouth were 84% of the annually averaged sediment discharge of the Zhujiang River,the annually averaged sediment discharges during the postglacial period and regressive phases would have been 9.91 and 15.35 Mt,respectively.
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