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距今5万年~1万年间浙江临安瑞晶洞穴石笋古温度记录

Paleotemperature Record of Stalagmite from Ruijing Cave, Lin' an County, Zhejiang Province,during the Period from 50000 to 10000 yrs B. P
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摘要 用稳定同位素地球化学古温度测定方法,对浙江省临安县瑞晶洞穴石笋进行了古温度研究,结果表明该地区在距今5万年~1万年间古温度有三次较明显的周期变化,最高温度为14.9℃,最低温度为6.6℃,最大温差为8℃左右,平均温差为3~5℃.用该方法测定的古温度研究结果与其它本法的古气候研究结果相一致. The paleotemperature of stalagmite,collected from Ruijing Cave, Lin'an County,Zhejiang Province,wasdetermined by using a stable-isotope geochemical method. The results show that during the period from50 000 to 10 000 yrs B. P.,the paleotemperature of study area had three-time obvious cyclic changes,andthat the highest temperature was 14. 9℃,the lowest 6. 6℃,the maximum temperature difference about 8℃,and the average temperature difference ranged from 3 to 5℃. The results are in keeping with the research results on paleoclimate obtained by using other methods.
出处 《科技通报》 1996年第5期257-261,共5页 Bulletin of Science and Technology
基金 国家自然科学基金
关键词 古温度 氧同位素 石笋 古气候 同位素地球化学 paleotemperature record, oxygen isotope, stalagmite
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  • 1杨子赓,李幼军,丁秋玲,何宝成.试论河北平原东部第四纪地质几个基本问题[J]地质学报,1979(04).

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