| 海州湾岸线变化特征 |
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| 引用本文： | 张传藻,葛殿铭.海州湾岸线变化特征[J].海洋科学,1982,6(3):11-17. |
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| 作者姓名： | 张传藻 葛殿铭 |
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| 作者单位： | 江苏连云港市档案局
(张传藻)，连云港建港指挥部(葛殿铭) |
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| 摘 要： | 海州湾位于黄海南部,除北端岚山头,南端连云港一带为基岩海岸外,其余为淤泥质平原海岸。 因区域构造差异,南北岸线变化表现不一,湾顶临洪口是过渡地段。本文着重探讨海州湾全新世特别是近一千年来海面变化特征及
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THE CHARACTERISTICS OF THE CHANGE OF THE HAI ZHOU GULF |
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| Abstract: | Most part of the Haizhou Culf is of silt-mud flat coast except the Lanshan Tou to the north and the Lianyun Port to the south.The coast line changes are various in the southern and northern coasts because of their geot-ectonic difference.Lin Hong Kou, which is located at the end of the Gulf is a transitional zone. In this paper, the characteristics of the change of sea level in Holocene, especially in the last 1000 years, are emphatically discussed. |
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