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| DOI | 10.1002/2014GC005252 |
| Stable isotopes of surface water across the Longmenshan margin of the eastern Tibetan Plateau | |
| Xu, Qiang; Hoke, Gregory D.; Jing Liu-Zeng; Ding, Lin; Wang, Wei; Yang, Yang | |
| 通讯作者 | Xu, Q (通讯作者) |
| 发表日期 | 2014 |
| EISSN | 1525-2027 |
| 起始页码 | 3416 |
| 结束页码 | 3429 |
| 卷号 | 15期号:8 |
| 英文摘要 | Characterization of the stable isotope compositions (O-18 and D) of modern-day surface waters traversing mountain ranges and bordering continental plateaus is important for refining climate models and establishing modern isotope-elevation gradients along mountain ranges. The Longmenshan margin of the Tibetan Plateau is a steep, 4 km topographic front situated near the boundaries between westerlies and Asian monsoon moisture sources, and is previously unexplored with respect to the variation in water isotopic composition with elevation. This study reports stable isotope data from 101 water samples collected from streams, springs, and ponds along the Min River (Minjiang) watershed, which traverses the Longmenshan margin. Local meteoric water lines, d-excess values, and surrounding precipitation and river water data sets suggest that precipitation across the Longmenshan margin is dominated by the East Asian summer monsoon. The increase in d-excess values with increasing catchment elevation breaks down as local moisture recycling becomes important at elevations>3 km a.s.l.. Along the Min River, however, the O-18(w) and D-w values decrease with increasing catchment elevation, which fit second-order polynomial curves and are well-approximated by a simple Rayleigh fractionation processes. The temperature-corrected oxygen values in authigenic carbonates from the Pleistocene Zoige Basin, north of the Min River watershed, yield elevations equivalent to present by the oxygen isotope-elevation relationship of the Longmenshan margin. |
| 关键词 | DEUTERIUM EXCESSDELTA O-18PRECIPITATIONPALEOELEVATIONPALEOALTIMETRYOXYGENUPLIFTPALEOCLIMATEMIOCENECLIMATE |
| 英文关键词 | stable isotopes; paleoelevation; Min River; Longmenshan margin; Tibetan Plateau |
| 语种 | 英语 |
| WOS研究方向 | Geochemistry & Geophysics |
| WOS类目 | Geochemistry & Geophysics |
| WOS记录号 | WOS:000342693400018 |
| 来源期刊 | GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
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| 来源机构 | 中国科学院青藏高原研究所 |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258378 |
| 推荐引用方式 GB/T 7714 | Xu, Qiang,Hoke, Gregory D.,Jing Liu-Zeng,et al. Stable isotopes of surface water across the Longmenshan margin of the eastern Tibetan Plateau[J]. 中国科学院青藏高原研究所,2014,15(8). |
| APA | Xu, Qiang,Hoke, Gregory D.,Jing Liu-Zeng,Ding, Lin,Wang, Wei,&Yang, Yang.(2014).Stable isotopes of surface water across the Longmenshan margin of the eastern Tibetan Plateau.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,15(8). |
| MLA | Xu, Qiang,et al."Stable isotopes of surface water across the Longmenshan margin of the eastern Tibetan Plateau".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 15.8(2014). |
| 条目包含的文件 | 条目无相关文件。 | |||||
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