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《Oceanologia Et Limnologia Sinica》 1978-01
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ON THE MARINE STRATIGRAPHY AND COASTLINES OF THE WESTERN COAST OF THE GULF OF BOHAI

Zhao Songling Yang Guangfu Cang Shuxi Zhang Hongcai Huang Qingfu (Institute of Oceanology,Academia Sinica)Xia Dongxing Wang Yongjie Liu Fushou Liu Chengfu (The First Institute of Oceanographical Research of the State Oceanography Bureau)  
Three marine formations are recognized from the Quaternary sediments(above 100 meters)of the western coast of the Gulf of Bohai. The C~(14) method and paleomagnetic measurements were used to estimate the age for each marine formation.The first marine formation existed between 102,000— 70,000 yrs B.P.belonging to Riss-Würm interglaciation.The second was between 39,000—23,000 yrs B.P.corresponding to the interstadial of Würm glaciation.The third was between 8000—2000 yrs B.P.corresponding to the postglacial deposition. The three marine formations indicated that three transgressive sequences occurred in the western coast of Bohai Gulf.The first transgression reached the vicinity of Xiegongting in the western part of Changzhou city,here termed Changzhou transgres- sion.The second transgression is greater in extent than the first,its boundary could reach Xianxian country,here termed XianXian transgression.The third transgression here termed Huanghua transgression,is less in extent than the first and the second, and is distributed only in the zone of Huanghua,Zhinghai,Tianjin(Tientsin).There- fore,we recognized three paleo-coastline in this area.
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