1. Crustal and Uppermost Mantle Azimuthal Seismic Anisotropy of Antarctica From Ambient Noise Tomography.
- Author
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Zhou, Zhengyang, Wiens, Douglas A., Nyblade, Andrew A., Aster, Richard C., Wilson, Terry, and Shen, Weisen
- Subjects
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SEISMIC anisotropy , *THEORY of wave motion , *SEISMIC waves , *RAYLEIGH waves , *INTERNAL structure of the Earth , *MONTE Carlo method - Abstract
Seismic anisotropy provides essential information for characterizing the orientation of deformation and flow in the crust and mantle. The isotropic structure of the Antarctic crust and upper mantle has been determined by previous studies, but the azimuthal anisotropy structure has only been constrained by mantle core phase (SKS) splitting observations. This study determines the azimuthal anisotropic structure of the crust and mantle beneath the central and West Antarctica based on 8—55 s Rayleigh wave phase velocities from ambient noise cross‐correlation. An anisotropic Rayleigh wave phase velocity map was created using a ray—based tomography method. These data are inverted using a Bayesian Monte Carlo method to obtain an azimuthal anisotropy model with uncertainties. The azimuthal anisotropy structure in most of the study region can be fit by a two‐layer structure, with one layer at depths of 0–15 km in the shallow crust and the other layer in the uppermost mantle. The azimuthal anisotropic layer in the shallow crust of West Antarctica, where it coincides with strong positive radial anisotropy quantified by the previous study, shows a fast direction that is subparallel to the inferred extension direction of the West Antarctic Rift System. Fast directions of upper mantle azimuthal anisotropy generally align with teleseismic shear wave splitting fast directions, suggesting a thin lithosphere or similar lithosphere‐asthenosphere deformation. However, inconsistencies in this exist in Marie Byrd Land, indicating differing ancient deformation patterns in the shallow mantle lithosphere sampled by the surface waves and deformation in the deeper mantle and asthenosphere sampled more strongly by splitting measurements. Plain Language Summary: Seismic anisotropy, which refers to the directional dependence of seismic wave propagation, provides crucial information about the orientation of deformation and flow within the interior of Earth. While most previous studies have focused on the isotropic structure, our study determines the azimuthal anisotropy structure beneath central and west Antarctica. We found that a two‐layer anisotropic structure fits the study region. In West Antarctica, the fast direction of the azimuthal anisotropy in the crust aligns with the extension direction of the West Antarctic Rift System. The agreement between our results and teleseismic core phase studies in the uppermost mantle suggests a thin lithosphere or similar lithosphere‐asthenosphere deformation. However, inconsistencies in certain areas of the study region, such as Marie Byrd Land, suggest that the deformation patterns differ between the shallow mantle lithosphere and the deeper mantle asthenosphere. These findings offer new insights into Antarctica's geological history. Key Points: Rayleigh wave phase velocities in Antarctica determined from ambient noise tomography have significant azimuthal anisotropyAnisotropy in the upper crust shows fast velocities that are subparallel to the inferred West Antarctic Rift System extension directionMantle fast velocities are often subparallel to core phase splitting directions, suggesting similar lithosphere‐asthenosphere anisotropy [ABSTRACT FROM AUTHOR]
- Published
- 2024
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