Lower crustal thickening drives active uplift in Northern Tibet

■Continuous GPS measurements reveal 1–2 mm/yr of uplift on the East Kunlun Shan with respect to the Qaidam Basin.■Hydrological loading, erosional unloading, glacial isostatic adjustment cannot explain the GPS-observed uplift.■Unrealistically large reverse-slip rate of 1.5–2.5 mm/yr is required to ex...

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Bibliographic Details
Published inEarth and planetary science letters Vol. 655; p. 119245
Main Authors Liu, Shaozhuo, Xu, Xiwei, Nocquet, Jean-Mathieu, Chen, Guihua, Tan, Xibin, Jónsson, Sigurjón, Klinger, Yann
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.04.2025
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