NIGPAS OpenIR  > 中国科学院南京地质古生物研究所
中中新世气候适宜期环境变化:来自中国西南部湖泊沉积地球化学的证据
Julie Lebreton-Anberrée; 李仕虎; 李树峰; Robert A.Spicer; 张世涛; 苏涛; 邓成龙; 周浙昆
2016
Source Publication科学通报
Volume61Issue:16Pages:1841
Indexed ByCSCD
Language中文
Document Type期刊论文
Identifierhttp://ir.nigpas.ac.cn/handle/332004/12520
Collection中国科学院南京地质古生物研究所
Recommended Citation
GB/T 7714
Julie Lebreton-Anberrée,李仕虎,李树峰,等. 中中新世气候适宜期环境变化:来自中国西南部湖泊沉积地球化学的证据[J]. 科学通报,2016,61(16):1841.
APA Julie Lebreton-Anberrée.,李仕虎.,李树峰.,Robert A.Spicer.,张世涛.,...&周浙昆.(2016).中中新世气候适宜期环境变化:来自中国西南部湖泊沉积地球化学的证据.科学通报,61(16),1841.
MLA Julie Lebreton-Anberrée,et al."中中新世气候适宜期环境变化:来自中国西南部湖泊沉积地球化学的证据".科学通报 61.16(2016):1841.
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