对我国沿海全新世海面变化研究的讨论  

Holocene sea-level change along China coast

作　　者：薛春汀[1] 

机构地区：[1]青岛海洋地质研究所,山东青岛266071

出　　处：《海洋学报》2002年第4期58-67,共10页

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.

关 键 词：全新世 海面变化 沉积环境 贝壳堤 庆丰剖面 中国 海岸 珊瑚礁 

分 类 号：P731.23[天文地球—海洋科学]