Sharp Lateral Moho Variations Across the SE Tibetan Margin and Their Implications for Plateau Growth. Issue 5 (14th May 2020)

• Record Type: Journal Article
• Authors: Xu, Mijian; Huang, Zhouchuan; Wang, Liangshu; Xu, Mingjie; Zhang, Yueqiao; Mi, Ning; Yu, Dayong; Yuan, Xiaohui
• Is Part Of: Journal of geophysical research. Volume 125:Issue 5(2020)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-05-14
• Subjects: Tibetan Plateau -- ChinArray -- receiver function -- Moho topography -- crustal flow; Geomagnetism -- Periodicals; Geochemistry -- Periodicals; Geophysics -- Periodicals; Earth sciences -- Periodicals; 551.1
• DOI: 10.1029/2019JB018117
• Languages: English
• ISSNs: 2169-9313

Abstract

Abstract: The tectonic uplift of the Tibetan Plateau is a focus in the geosciences. Middle‐lower crustal flow is a popular model to interpret the geodynamic mechanism on the margin of the Tibetan Plateau. The model predicts different surface and Moho topographies across the plateau boundary due to the different strengths of the surrounding blocks, that is, sharp boundaries on the eastern plateau boundary and gentle variations in the southeastern plateau boundary. Here, we employ receiver function and common conversion point stacking analysis with the seismic waveforms recorded by the dense ChinArray and other local seismic stations to accurately define the Moho topography in southeastern (SE) Tibet. We find that the Moho under the Tibetan Plateau is much deeper than that under the surrounding Yangtze Craton and Indochina block; abrupt Moho changes are found across the southeastern plateau margin, similar to that under the eastern plateau margin. We interpret these sharp Moho variations across the plateau margin to have developed when the Tibetan Plateau was extruded southeastward in the late Miocene. Subsequent gravity collapse resulted in crustal extension and gentle topographic variation, while the sharp Moho slope was preserved. Key Points: We mapped the Moho depths under SE Tibet revealed by receiver function analysis Large Moho depth gradients are found beneath the boundary faults along the SE Tibetan margin The evolution of SE Tibet involved crustal thickening during block extrusion and subsequent surface topography smoothing by gravity collapse