摘要
用稳定同位素地球化学古温度测定方法对杭州临安瑞晶洞穴石笋的同位素古温度进行了研究，获得了距今（5～1）×104a间该区的古气候演化记录，并与杭州湾海平面变化曲线进行了对比。
The stable isotopes carbon, hydrogen and oxygen in the stalagrnites from the Ruijing Cave,Linan, Zhriiang, were determined by the method of stable lsotope geochemistry. The records of paleoclimate evolution in the Rujing Cave (5 ×104 ～ 1 ×104 a) have been obtained and are compared withthe curve of sea level change of the Hangzhou Bay.
出处
《地质地球化学》
CSCD
北大核心
1998年第1期37-40,共4页
Geology-Geochemistry
基金
中科院西安黄土与第四纪开放实验室资助
