摘要
通过对研究区内三个典型钻孔岩芯的沉积相识别标志的综合分析,并对比研究区内其它地方近百个钻孔岩性资料,确定了划分全新世和更新世的标志层,论述了温州湾地区全新世以来的沉积环境演变和气候变迁过程。
Based upon the fieldwork and the synthetical analysis of sedimentary facies of three typical sections and nearly 100 drilling cores available in the area, the paper expounds the evolution of Holecene sedimentary environment and the process of climate change in Wenzhou Bay.
出处
《西北师范大学学报（自然科学版）》
CAS
1991年第4期71-77,共7页
Journal of Northwest Normal University(Natural Science)
关键词
全新世
沉积环境
温州湾地区
sedimentary environment, climate change, Holecene, Wenzhou Bay
