Weilong Rao , Bin Liu , Tengfei Feng , Qiuyu Wang , He Tang
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引用次数: 0
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 ± 0.32 mm/yr, which is smaller than the 0.46 ± 0.08 mm/yr contributed by loading and glacial isostatic adjustment (GIA).
期刊介绍:
Earth and Planetary Science Letters (EPSL) is a leading journal for researchers across the entire Earth and planetary sciences community. It publishes concise, exciting, high-impact articles ("Letters") of broad interest. Its focus is on physical and chemical processes, the evolution and general properties of the Earth and planets - from their deep interiors to their atmospheres. EPSL also includes a Frontiers section, featuring invited high-profile synthesis articles by leading experts on timely topics to bring cutting-edge research to the wider community.