摘要
距今 6 0 0 0a的高海面及其后海面波动论点的主要依据是对渤海西岸贝壳堤、华南海岸海滩岩和珊瑚礁、天津市宁河县口牡蛎礁剖面和江苏北部建湖县庆丰剖面的研究 ,然而这些资料无法证明高海面和海面波动 ,因为珊瑚礁、牡蛎礁、贝壳堤。
The bases of the viewpoint of higher sea level in 6 000 aBP and sea level fluctuation since then are the shell ridges on the west coast of the Bohai Sea, beachrock and coral reefs on South China coast, the Holocene stratigraphic section at Biaokou Village, Ninghe County, Tianjin Municipality and Qingfeng section in Jianhu County, Jiangsu Province. However, the above data cannot provide such evidences, because the coral reef, oyster reef, shell ridge, beachrock and tidal flat deposits cannot provide information of such accurate sea level changes.
出处
《海洋学报》
CAS
CSCD
北大核心
2002年第4期58-67,共10页
