Crust and upper mantle shear velocity structure beneath the Tibetan plateau and surrounding regions from interevent surface wave phase velocity inversion
Average a priori shear velocity models are constructed for the Tien Shan, Tarim basin, Pamir-Hindu Kush, Himalaya and NE India. These models are shown to account for most of the lateral velocity heterogeneity at wavelengths > 1000 km. Interevent fundamental mode Rayleigh and Love wave phase v...
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| Format: | Journal article |
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1997
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