IEECAS OpenIR  > 黄土与第四纪地质国家重点实验室(2005-2009)
黄土高原现代自然降尘的特征——以固原安塞为例
梁剑鸣; 周杰; 何忠; 刘卫国; 梁银丽; 程积民
2009
Source Publication海洋地质与第四纪地质
Issue1Pages:103-108
Cooperation Status其它
Keyword降尘 有机碳 粒度 磁化率 黄土高原
Subject Area环境科学
Language中文
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/1763
Collection黄土与第四纪地质国家重点实验室(2005-2009)
Recommended Citation
GB/T 7714
梁剑鸣,周杰,何忠,等. 黄土高原现代自然降尘的特征——以固原安塞为例[J]. 海洋地质与第四纪地质,2009(1):103-108.
APA 梁剑鸣,周杰,何忠,刘卫国,梁银丽,&程积民.(2009).黄土高原现代自然降尘的特征——以固原安塞为例.海洋地质与第四纪地质(1),103-108.
MLA 梁剑鸣,et al."黄土高原现代自然降尘的特征——以固原安塞为例".海洋地质与第四纪地质 .1(2009):103-108.
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