摘要
郑州市区面积约970km^2,发育一套河湖相全新世地层。笔者在前人工作的基础上,将该套地层作了较为详细分层。文中化石由严富华、蓝朝玉、付茂兰(孢粉),王景哲(介形类),郭书元(腹足类),王新海(轮藻),鉴定,热发光测定(计风桔),^(14)C年龄由中国科学院贵阳地球化学研究所^(14)C组和中国社会科学院考古研究所完成。野外工作期间得到海贤智、袁宝玉等同志协助,在此致谢。
Based on the field investigation and drill log and experimental results as well as other data, several type sections are described in this paper. The principles of stratigraphic division and correlation are discussed also. Holocene series in Zhengzhou may be divided into three formations: (1) Lower Holocene Dali (11000-7500 years), (2) Middle Holocene Dahe-cun (7500-2500 years) and (3) Upper Holocene Putian (2500-present).
出处
《地层学杂志》
CSCD
北大核心
1992年第2期111-119,共9页
Journal of Stratigraphy
