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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Published in | Earth and planetary science letters Vol. 655; p. 119245 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
01.04.2025
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Subjects | |
Online Access | Get full text |
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