Lithospheric dynamics in the vicinity of the Tengchong volcanic field (southeastern margin of Tibet): an investigation using P receiver functions. Issue 2 (29th October 2020)

• Record Type: Journal Article
• Authors: Peng, Hengchu; Badal, José; Hu, Jiafu; Yang, Haiyan; Liu, Benyu
• Is Part Of: Geophysical journal international. Volume 224:Issue 2(2021)
• Page Start: 1326
• Page End: 1343
• Publication Date: 2020-10-29
• Subjects: Crustal imaging -- Seismic anisotropy -- Dynamics of lithosphere and mantle -- Kinematics of crustal and mantle deformation -- Magma migration and fragmentation; Geophysics -- Periodicals; 550
• DOI: 10.1093/gji/ggaa517
• Languages: English
• ISSNs: 0956-540X

Abstract

SUMMARY: Tengchong volcanic field (TVF) in the northern Indochina block lies in a critical area for understanding complex regional dynamics associated with continent–continent convergence between the Indian and Eurasian plates, including northeastward compression generated by subduction of the Indian Plate beneath the Burma Arc, and southeastward lateral extrusion of the crust from below central Tibet. We gathered 3408 pairs of P receiver functions with different frequencies and calculated the splitting parameters of the Moho-converted Pms phase. An anisotropic H - κ stacking algorithm was used to determine crustal thickness and Vp/Vs ratios. We also inverted for the detailed S -velocity structure of the crust and upper mantle using a two-step inversion technique. Finally, we mapped the topography of the lithosphere–asthenosphere boundary. Results show fast-wave polarization directions with a dominant NE–SW orientation and delay times varying between 0.19 and 1.22 s, with a mean of 0.48 ± 0.07 s. The crustal Vp/Vs ratio varies from 1.68 to 1.90 and shows a maximum value below the central part of the TVF, where there is relatively thin crust (∼35–39 km) and a pronounced low-velocity anomaly in the middle–lower crust. The depth of the lithosphere–asthenosphere boundary ranges from 53 to 85 km: it is relatively deep (∼70–85 km) in the vicinity of the TVF and relatively shallow in the south of the study area. In the absence of low shear wave velocity in the upper mantle below the TVF, we propose that the low-velocity anomaly in the lower crust beneath the TVF derives from the upper mantle below the neighbouring Baoshan block.