Rayleigh wave tomography of central and southern Mongolia

The Mongolian Plateau located between the Siberian Craton and the North China Craton developed after multiple tectonic evolutions. It is proposed to be related to the far-field effect of the Indo-Asian collision in the Cenozoic. In this study, we inverted for high-resolution S wave velocity structur...

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Veröffentlicht in:	Tectonophysics 2022-08, Vol.836, p.229426, Article 229426
Hauptverfasser:	Wang, Xinglu, Wu, Hanting, Wang, Haibo, Wu, Benjun, Huang, Zhouchuan
Format:	Artikel
Sprache:	eng
Schlagworte:	Anomalies Cenozoic Cratons Deserts Domes Far fields Geological faults Gobi Desert Historical structures Isotopes Mantle upwelling Mongolia Ocean circulation Paleozoic Rayleigh waves S waves Seismic velocities Slabs Subduction (geology) Surface-wave tomography Suture zones Tectonics Tomography Upper mantle Upwelling Velocity Wave velocity
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