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	Palaeoclimatic evolution recorded by multidicipline in sediments in gahai lake, qaidam basin since late last deglacial
	Chen Zhong[1,2]; Ma Haizhou[2]; Cao Guangchao[3]; Zhang Xiying[2]; Zhou Dujun[2]; Yao Yuan[4]; Yang Guangshu[1]
	2010
卷号	16期号:3页码:324
关键词	古气候演化 冰消期 尕海湖 盆地沉积物 柴达木 早全新世 碳酸盐含量 沉积特征
URL标识	查看原文
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/5859594
专题	青海师范大学
作者单位	1.[1]Faculty of Land Resource Engineering, Kunming University of Science and Technology, Kunming 650093, P.R. China 2.[2]Qinghai Institute of Salt Lake, Chinese Academy of Sciences, Xining 810008, P.R. China 3.[3]School of Life and Geography Science, Qinghai Normal University, Xining 810008, P.R. China 4.[4]East China Geological Exploration Institute of Non-ferrous Metals, Nanjing 210007, P.R. China
推荐引用方式 GB/T 7714	Chen Zhong[1,2],Ma Haizhou[2],Cao Guangchao[3],et al. Palaeoclimatic evolution recorded by multidicipline in sediments in gahai lake, qaidam basin since late last deglacial[J],2010,16(3):324.
APA	Chen Zhong[1,2].,Ma Haizhou[2].,Cao Guangchao[3].,Zhang Xiying[2].,Zhou Dujun[2].,...&Yang Guangshu[1].(2010).Palaeoclimatic evolution recorded by multidicipline in sediments in gahai lake, qaidam basin since late last deglacial.,16(3),324.
MLA	Chen Zhong[1,2],et al."Palaeoclimatic evolution recorded by multidicipline in sediments in gahai lake, qaidam basin since late last deglacial".16.3(2010):324.

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