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《Transactions of Oceanology and Limnology》 1987-02
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HOLOCENE TRANSGRESSION AND ITS LAYERS IN THE EAST COAST OF LAIZHOU GULF, BOHAI

Zhuang Zhenye;Li Jian-hua;Qiu Shihua;Xian Ziqiang;Bao Guancheng;Wang Yongji Shandong College of Oceanology Institute of Archaeology, CASS. First Institute of Oceanography, NBO  
The lagoon--sea plain about 200 KM~2 in the east coast area of Laizhou Gulf. Bohai was formed by the Holocene transgression. The marine layer consists of blue grey silt-fine sand, in which there are many shells, shell clastics and Foraminifera Its underlying and overlying layers are alluvial deposits respectively formed during the late Pleistocene and late Holocene. We call this transgression in this place "Laizhou Transgression". The largest transgression took place at about 6, 000 yers (B. P.) or so. The sea level in this period was higher than present. A pleoshoreline about 80 KM. was remained in the plain.
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