摘要
本文通过对浙江沿岸浅水区5个钻孔岩芯的底栖有孔虫分析,并结合^(14)C、孢粉和浅地层等分析资料,主要讨论该地区晚更新世末期40000年以来的沉积环境、海侵层厚度和海面变化过程等问题。
In this paper, benthic foraminifera is determined in five drill cores in the littoral-shallow water areas of Zhejiang province. Combining with the analytical data of 14C, spore-pollen and profiling survey of shallow layer, the sedimentary environment, thicknesses of ingression layers, and processes of sea-level changes for this area are discussed since late Plaistocene (40000 years B. P.).
出处
《东海海洋》
1989年第2期24-32,共9页
Donghai Marine Science
