Late Cretaceous–Cenozoic basin evolution and topographic growth of the Hoh Xil Basin, central Tibetan Plateau

2017 ◽  
Vol 130 (3-4) ◽  
pp. 499-521 ◽  
Author(s):  
Lin Li ◽  
Carmala N. Garzione ◽  
Alex Pullen ◽  
Peng Zhang ◽  
Yun Li
Keyword(s):  
Tibetan Plateau ◽  
Late Cretaceous ◽  
Basin Evolution ◽  
Central Tibetan Plateau

Ice-core based assessment of nitrogen deposition in the central Tibetan Plateau over the last millennium

2021 ◽  
pp. 152692
Author(s):  
Xiang Zou ◽  
Shugui Hou ◽  
Shuangye Wu ◽  
Hongxi Pang ◽  
Ke Liu ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Nitrogen Deposition ◽  
Ice Core ◽  
Last Millennium ◽  
Central Tibetan Plateau

scholarly journals Facilitation stabilizes moisture-controlled alpine juniper shrublines in the central Tibetan Plateau

2015 ◽  
Vol 132 ◽  
pp. 20-30 ◽  
Author(s):  
Yafeng Wang ◽  
Eryuan Liang ◽  
Aaron M. Ellison ◽  
Xiaoming Lu ◽  
J. Julio Camarero
Keyword(s):  
Tibetan Plateau ◽  
Central Tibetan Plateau

Impact of Drought Stress on Net CO2Exchange Above an Alpine Grassland Ecosystem in the Central Tibetan Plateau

2013 ◽  
Vol 4 (4) ◽  
pp. 327-336 ◽  
Author(s):  
Zhao Yuping ◽  
Zhang Xianzhou ◽  
Shi Peili ◽  
Wang Jingsheng ◽  
Wu Jianshuang
Keyword(s):  
Drought Stress ◽  
Tibetan Plateau ◽  
Alpine Grassland ◽  
Grassland Ecosystem ◽  
Central Tibetan Plateau ◽  
Alpine Grassland Ecosystem

scholarly journals Luminescence dating of lacustrine sediments from CUOE Lake on the central Tibetan Plateau

2020 ◽  
Vol 0 (0) ◽  
Author(s):  
Yandong Hou ◽  
Hao Long ◽  
Lei Gao ◽  
Ji Shen
Keyword(s):  
Tibetan Plateau ◽  
Lacustrine Sediments ◽  
Water Reservoir ◽  
Hard Water ◽  
Luminescence Dating ◽  
Coarse Grained ◽  
The Tibetan Plateau ◽  
Sediment Layer ◽  
Central Tibetan Plateau ◽  
Dating Method

AbstractLuminescence dating technology has been used for chronological constraints on lacustrine sediments due to the ubiquitous materials (e.g., quartz and feldspar) as dosimeters, and a relatively long dating range, compared with the commonly used radiocarbon dating method. However, quartz dating on the Tibetan Plateau may suffer from dim and unstable luminescence signals. In the current study, we investigate a lake-related outcrop from the shore of Cuoe Lake on the central Tibetan Plateau. Both coarse-grained quartz and K-feldspar fractions were extracted, and OSL and post-IR IRSL signals were measured from these fractions, respectively. Combining the stratigraphy analysis and dating results, this study shows that: (1) quartz appears to be unsuitable for dating because of very dim natural signals and even anomalous fading (average g-value: 4.30 ± 2.51 %/decade). The suitability of the applied pIRIR protocol measured at 150°C (pIRIR150) for K-feldspar samples was confirmed by a set of luminescence tests; (2) compared with the luminescence-based chronology, the 14C age of shells from the same sediment layer yielded older age by ~7 ka, which is likely attributed to hard water reservoir effect in Cuoe Lake; (3) the lake level reached its peak and maintained high-stand during the early Holocene (~9.4–7.1 ka). This study highlights the applicability of K-feldspar luminescence dating when the counterpart quartz OSL is insensitive and encounters anomalous fading.

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