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Zhang Hunan,Zhao Hongmei.Preliminary research on sea-level changes of the South China coast since late Epipleistocene[J].Acta Oceanologica Sinica,1991,(4):565-591
Preliminary research on sea-level changes of the South China coast since late Epipleistocene
Preliminary research on sea-level changes of the South China coast since late Epipleistocene
投稿时间:1990-06-13  修订日期:1990-12-25
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作者单位
Zhang Hunan Seismological Bureau of Guangdong Province, Guangzhou 510070, China 
Zhao Hongmei Seismological Bureau of Guangdong Province, Guangzhou 510070, China 
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中文摘要:
      Several views on sea-level changes of the South China coast are briefly introduced in this paper. On the basis of 236 samples whose ages are determined by 14C chronological method and their sites are corrected with ancient water depth and crustal deformation, a basic model about sea-level changes of the South China coast since late Epipleistocene is set up. This model basically accords with the general cognitions of predecessors, i.e. it not only represents the common characteristics of sea-level changes of the East China coast but has some features of the South China coast itself. In general, this model is relatively close to the Fairbridge's curve, indicating that the sea-level undulations exist since 6 ka ago but the ranges of undulations are slightly larger than those of Fairbridge's curve.
英文摘要:
      Several views on sea-level changes of the South China coast are briefly introduced in this paper. On the basis of 236 samples whose ages are determined by 14C chronological method and their sites are corrected with ancient water depth and crustal deformation, a basic model about sea-level changes of the South China coast since late Epipleistocene is set up. This model basically accords with the general cognitions of predecessors, i.e. it not only represents the common characteristics of sea-level changes of the East China coast but has some features of the South China coast itself. In general, this model is relatively close to the Fairbridge's curve, indicating that the sea-level undulations exist since 6 ka ago but the ranges of undulations are slightly larger than those of Fairbridge's curve.
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