Knowledge Management System Of Guangzhou Institute of Geochemistry，CAS
| Houyun Z; Zhaoyu Z | |
| Oxygen isotopic composition of lacustrine carbonates since 130 ka BP from a Tianshuihai Lake core, Tibet: an overall increasing delta O-18 trend and its implications | |
| Source Publication | Journal of Asian Earth Sciences
 |
| ISSN | 1367-9120 |
| 2002 | |
| Volume | 20Issue:3Pages:225-229 |
| Language | 英语 |
| WOS ID | WOS:000172661900005 |
| Indexed By | sci |
| Citation statistics | |
| Document Type | 期刊论文 |
| Identifier | http://ir.gig.ac.cn/handle/344008/11899 |
| Collection | 中科院广州地化所(-2008) |
| Recommended Citation GB/T 7714 | Houyun Z,Zhaoyu Z. Oxygen isotopic composition of lacustrine carbonates since 130 ka BP from a Tianshuihai Lake core, Tibet: an overall increasing delta O-18 trend and its implications[J]. Journal of Asian Earth Sciences,2002,20(3):225-229. |
| APA | Houyun Z,&Zhaoyu Z.(2002).Oxygen isotopic composition of lacustrine carbonates since 130 ka BP from a Tianshuihai Lake core, Tibet: an overall increasing delta O-18 trend and its implications.Journal of Asian Earth Sciences,20(3),225-229. |
| MLA | Houyun Z,et al."Oxygen isotopic composition of lacustrine carbonates since 130 ka BP from a Tianshuihai Lake core, Tibet: an overall increasing delta O-18 trend and its implications".Journal of Asian Earth Sciences 20.3(2002):225-229. |
| Files in This Item: | ||||||
| File Name/Size | DocType | Version | Access | License | ||
| 02035.pdf（103KB） | 暂不开放 | -- | Application Full Text | |||
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