DEPOSITIONAL CHARACTERISTICS OF THE SYSTEM OFSAND-GRAVEL OUTER BAR AND LAGOON ANDEUSTASY IN HOLOCENE IN LIAONINGCOASTAL ZONE
辽宁海岸沙砾堤—潟湖体系沉积特征与全新世海面变化

Changs' of sedimentary environment of the system of sand-gravel outer bar and lagoon in Liaoning coastal zone illustrated that the rising of temperature in the postglacial period had caused that of sea level. Since 9000 B.P. sea water has transgressed into this zone, and the sea level in the period of 8000-7000 B.P. was 1.5-2.5 m higher than that of present. Since 5000 B.P. it has tended to descend and experienced fluctuating and relative stable periods.