scholarly journals Crustal Azimuthal Anisotropy Beneath the Southeastern Tibetan Plateau and its Geodynamic Implications

2018 ◽  
Vol 123 (11) ◽  
pp. 9733-9749 ◽  
Author(s):  
Tuo Zheng ◽  
Zhifeng Ding ◽  
Jieyuan Ning ◽  
Lijun Chang ◽  
Xingchen Wang ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Azimuthal Anisotropy ◽  
Southeastern Tibetan Plateau

scholarly journals Role of the Early Miocene Jinhe-Qinghe Thrust Belt in the building of the Southeastern Tibetan Plateau topography

2021 ◽  
Vol 811 ◽  
pp. 228871
Author(s):  
Chengyu Zhu ◽  
Guocan Wang ◽  
Philippe Hervé Leloup ◽  
Kai Cao ◽  
Gweltaz Mahéo ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Early Miocene ◽  
Thrust Belt ◽  
Southeastern Tibetan Plateau

scholarly journals Linking deeply-sourced volatile emissions to plateau growth dynamics in southeastern Tibetan Plateau

2021 ◽  
Vol 12 (1) ◽  
Author(s):  
Maoliang Zhang ◽  
Zhengfu Guo ◽  
Sheng Xu ◽  
Peter H. Barry ◽  
Yuji Sano ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Growth Dynamics ◽  
High Elevation ◽  
Fault System ◽  
The Tibetan Plateau ◽  
Southeastern Tibetan Plateau ◽  
Surface Uplift ◽  
Multi Stage ◽  
Geodynamic Processes ◽  
Underlying Mechanisms

AbstractThe episodic growth of high-elevation orogenic plateaux is controlled by a series of geodynamic processes. However, determining the underlying mechanisms that drive plateau growth dynamics over geological history and constraining the depths at which growth originates, remains challenging. Here we present He-CO2-N2 systematics of hydrothermal fluids that reveal the existence of a lithospheric-scale fault system in the southeastern Tibetan Plateau, whereby multi-stage plateau growth occurred in the geological past and continues to the present. He isotopes provide unambiguous evidence for the involvement of mantle-scale dynamics in lateral expansion and localized surface uplift of the Tibetan Plateau. The excellent correlation between 3He/4He values and strain rates, along the strike of Indian indentation into Asia, suggests non-uniform distribution of stresses between the plateau boundary and interior, which modulate southeastward growth of the Tibetan Plateau within the context of India-Asia convergence. Our results demonstrate that deeply-sourced volatile geochemistry can be used to constrain deep dynamic processes involved in orogenic plateau growth.

Rapid glacier mass loss in the Southeastern Tibetan Plateau since the year 2000 from satellite observations

2022 ◽  
Vol 270 ◽  
pp. 112853
Author(s):  
Fanyu Zhao ◽  
Di Long ◽  
Xingdong Li ◽  
Qi Huang ◽  
Pengfei Han
Keyword(s):  
Tibetan Plateau ◽  
Mass Loss ◽  
Satellite Observations ◽  
Southeastern Tibetan Plateau ◽  
Year 2000

A 400-year tree-ring δ18O chronology for the southeastern Tibetan Plateau: Implications for inferring variations of the regional hydroclimate

2013 ◽  
Vol 104 ◽  
pp. 23-33 ◽  
Author(s):  
Xiaohong Liu ◽  
Xiaomin Zeng ◽  
Steven W. Leavitt ◽  
Wenzhi Wang ◽  
Wenling An ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
Tree Ring ◽  
Southeastern Tibetan Plateau
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