• Sorted by Date • Sorted by Last Name of First Author •
Rao, Weilong, Liu, Bin, Feng, Tengfei, Wang, Qiuyu, and Tang, He, 2025. What is the present-day tectonic uplift rate of the Tibetan Plateau?. Earth and Planetary Science Letters, 662:119389, doi:10.1016/j.epsl.2025.119389.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025EPSL.66219389R, author = {{Rao}, Weilong and {Liu}, Bin and {Feng}, Tengfei and {Wang}, Qiuyu and {Tang}, He}, title = "{What is the present-day tectonic uplift rate of the Tibetan Plateau?}", journal = {Earth and Planetary Science Letters}, year = 2025, month = jul, volume = {662}, eid = {119389}, pages = {119389}, abstract = "{The Tibetan Plateau (TP) exhibits millimeter-scale vertical crustal deformation, detected through Global Positioning System (GPS) measurements. Concurrently, significant terrestrial water loss in High Mountain Asia contributes to plateau uplift via hydrological loading. After accounting for loading-induced uplift, it remains unclear whether the TP continues to experience significant tectonic uplift. To resolve this, a global hydrological mass change field was reconstructed using satellite observations and hydrological models, rather than relying on the Gravity Recovery and Climate Experiment (GRACE) data, to quantify vertical loading displacement rates for correcting GPS vertical velocities. Furthermore, a GPS imaging technique that incorporates the spatial structure function (SSF) was used to generate a tectonic deformation image of the TP. The results indicate that the TP is not experiencing uniform and significant tectonic uplift; instead, regional crustal subsidence is observed. The mean tectonic uplift rate is only 0.31 {\ensuremath{\pm}} 0.32 mm/yr, which is smaller than the 0.46 {\ensuremath{\pm}} 0.08 mm/yr contributed by loading and glacial isostatic adjustment (GIA).}", doi = {10.1016/j.epsl.2025.119389}, adsurl = {https://ui.adsabs.harvard.edu/abs/2025E&PSL.66219389R}, adsnote = {Provided by the SAO/NASA Astrophysics Data System} }
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