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• W4379513283 abstract "Shear wave splitting measurement of teleseismic data has been used to determine the fast polarization directions and delay times for 38 temporary stations and 15 permanent stations from a NW linear seismic array across the eastern Tarim basin (ETB) and the northern Tibetan Plateau (NTP), and 10 permanent stations on both sides of the array. We present an image of upper mantle anisotropy in the ETB and NTP using the 63 new measurements. The results show that the fast directions and delay times have complex spatial distribution characteristics. The delay times within the interior of the Tarim basin are very small, with an average value of 0.6 s, which is not only smaller than that in the Altyn Tagh fault and Tianshan on the southern and northern margins of the basin, but also smaller than that in the NTP, reflecting that the delay time of stable blocks is smaller than that of active blocks. Along the array, from east to west, the fast directions contrarotate from NNW in the southern Songpan-Garze terrane to NW in the northern Songpan-Garze terrane, to near E-W or ENE in the north of the East Kunlun fault and southern margin of the Qaidam basin, then first abruptly rotate to NW in the Qiman Tagh fault on the northwestern margin of the Qaidam basin, second abruptly rotate to ENE in the Altyn Tagh fault and south of the ETB, and third abruptly rotate to NW in the north of the ETB, then finally rotate to WNW in the Tianshan. The comparative analysis between the fast wave directions measured by shear wave splitting and predicted from the surface deformation field shows that, with the exclusion of the five observations with larger misfits within the interior of the ETB (with an average misfit of 27°), the misfits in the NTP and northern and southern margins of the Tarim basin are relatively small (with an average misfit of 9°). In addition, the fast wave directions of the tectonic units such as the Altyn Tagh fault, East Kunlun fault, and Tianshan are parallel to the strikes of faults and mountains in the region, which indicates that the deep and shallow deformations of the NTP and northern and southern margins of the ETB are consistent, where the crust-mantle coupling extent of lithospheric deformation is higher, according with the vertical coherent deformation of the lithosphere. Conversely, the crust-mantle coupling extent within the interior of the Tarim Basin is weak, and it is characterized by weak anisotropy, stable rigidity, and thick lithosphere, which may remain the “fossil” anisotropy of ancient craton." @default.
• W4379513283 created "2023-06-07" @default.
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• W4379513283 date "2023-06-02" @default.
• W4379513283 modified "2023-09-24" @default.
• W4379513283 title "Teleseismic shear wave splitting and intracontinental collision deformation of the northern Tibetan Plateau and the eastern Tarim basin" @default.
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• W4379513283 doi "https://doi.org/10.1007/s11430-022-1068-5" @default.
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