GIG OpenIR  > 同位素地球化学国家重点实验室
黄龙[1,2,3,4]; 陈怡伟[1,2,3]; 吴洋[1,2,3,4]; 崔灏[1,2,3,4]; 韦刚健[1,2,3]; 曾提[1,2,3]
西藏佩枯错早全新世以来湖泊退缩过程及其古环境意义
Source Publication地球化学
ISSN0379-1726
2023
Volume52Issue:4Pages:448-457
Language中文
Indexed ByCSCD
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Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/70186
Collection同位素地球化学国家重点实验室
Affiliation1.中国科学院广州地球化学研究所,同位素地球化学国家重点实验室,广东广州510640
2.中国科学院深地科学卓越创新中心,广东广州510640
3.南方海洋科学与工程广东省实验室(广州),广东广州511458
4.中国科学院大学地球与行星科学学院,北京100049
Recommended Citation
GB/T 7714
黄龙[1,2,3,4],陈怡伟[1,2,3],吴洋[1,2,3,4],等. 西藏佩枯错早全新世以来湖泊退缩过程及其古环境意义[J]. 地球化学,2023,52(4):448-457.
APA 黄龙[1,2,3,4],陈怡伟[1,2,3],吴洋[1,2,3,4],崔灏[1,2,3,4],韦刚健[1,2,3],&曾提[1,2,3].(2023).西藏佩枯错早全新世以来湖泊退缩过程及其古环境意义.地球化学,52(4),448-457.
MLA 黄龙[1,2,3,4],et al."西藏佩枯错早全新世以来湖泊退缩过程及其古环境意义".地球化学 52.4(2023):448-457.
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