通过对钻孔岩心和浅地层地震剖面的分析，恢复了辽东湾北部晚更新世中期以来的沉积环境。
The deposit environment in the north of Liaodong Bay since the medium-term of late Pleistocene is rebuilt by the analyses of the core and the seismic profile.
自渤海湾和辽东湾一线向渤海海峡盐度逐渐降低，高盐度区出现在渤海湾东部和辽东湾北部。
Salinity decreased from the Bohai Bay and the Liaodong Bay to the Bohai Strait. The high values of salinity were mostly concentrated in the east of Bohai Bay and the north of Liaodong Bay.
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