Lateral Growth Mechanism of Proto‐Tibetan Plateau in the Late Paleogene: Implications From Detailed Crustal Structures of the Hoh Xil Basin
Author:
Affiliation:
1. Chinese Academy of Geological Sciences Beijing China
2. Deutsches GeoForschungsZentrum Potsdam Germany
3. Institute of Geology and Geophysics Chinese Academy of Sciences Beijing China
Funder
National Natural Science Foundation of China
Deutsche Forschungsgemeinschaft
China Postdoctoral Science Foundation
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL097983
Reference59 articles.
1. The isolation of receiver effects from teleseismic P waveforms
2. Early‐Stage Lithospheric Foundering Beneath the Eastern Tibetan Plateau Revealed by Full‐Wave P n Tomography
3. Velocities and propagation characteristics of Pn and Sn beneath the Himalayan arc and Tibetan plateau: Possible evidence for underthrusting of Indian continental lithosphere beneath Tibet
4. Observations of frequency-dependentSnpropagation in Northern Tibet
5. A “no-lid” zone in the central Chang-Thang platform of Tibet: Evidence from pure path phase velocity measurements of long period Rayleigh waves
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