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Azimuthal Anisotropy and Mantle Flow Underneath the Southeastern Tibetan Plateau and Northern Indochina Peninsula Revealed by Shear Wave Splitting Analyses
Tectonophysics
  • Fansheng Kong
  • Jing Wu
  • Lin Liu
  • Kelly H. Liu, Missouri University of Science and Technology
  • Jianguo Song
  • Jiabiao Li
  • Stephen S. Gao, Missouri University of Science and Technology
Abstract

Seismic azimuthal anisotropy beneath the transitional region between the southeastern Tibetan Plateau and the Indochina Peninsula, an area in which the fast orientation of mantle anisotropy changes to dominantly E-W from mostly N-S on the plateau at the north, is quantified using splitting of the SKS, SKKS, and PKS phases. Among the 50 stations with one or more splitting measurements, 22 possess an azimuthal coverage that is adequate for the identification and characterization of complex anisotropy. The resulting splitting parameters from 15 such stations exhibit systematic back azimuthal variations with a 90° periodicity, which is consistent with a two-layered anisotropy model. The upper layer parameters are consistent with crustal anisotropy measurements obtained independently based on the sinusoidal moveout of P-to-S conversions from the Moho, with the fast orientations being mostly parallel to major shear zones. The lower layer fast orientations and the fast orientations at stations with azimuthally invariant splitting parameters are mostly E-W, which is significantly different from the dominantly N-S trend of the surface expression of major structural fabrics in the area. They are also inconsistent with the absolute plate motion directions. When combined with results from seismic tomography and focal mechanism solutions, the observed azimuthal anisotropy can be adequately explained by the movement of the lithosphere relative to the underlain asthenosphere, most likely associated with the westward rollback of the subducted Indian Plate.

Department(s)
Geosciences and Geological and Petroleum Engineering
Comments

The study was partially supported by grant no. HYGG1802 of the Scientific Research Fund of the Second Institute of Oceanography State Oceanic Administration of China to F.K., and the United States National Science Foundation grants EAR-0911346 , EAR-1321656 , and EAR-1830644 to K.L. and S.G.

Keywords and Phrases
  • Seismic anisotropy,
  • Shear wave splitting,
  • Slab rollback,
  • Southeastern Tibetan Plateau
Document Type
Article - Journal
Document Version
Citation
File Type
text
Language(s)
English
Rights
© 2018 Elsevier, All rights reserved.
Publication Date
11-1-2018
Disciplines
Citation Information
Fansheng Kong, Jing Wu, Lin Liu, Kelly H. Liu, et al.. "Azimuthal Anisotropy and Mantle Flow Underneath the Southeastern Tibetan Plateau and Northern Indochina Peninsula Revealed by Shear Wave Splitting Analyses" Tectonophysics Vol. 747-748 (2018) p. 66 - 78 ISSN: 0040-1951; 1879-3266
Available at: http://works.bepress.com/kelly-liu/125/