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- W2007751710 abstract "Earthquake data collected by the INDEPTH-II Passive-Source Experiment show that there is a substantial south to north variation in the velocity structure of the crust beneath southern Tibet. North of the Zangbo suture, beneath the southern Lhasa block, a midcrustal low-velocity zone is revealed by inversion of receiver functions, Rayleigh-wave phase velocities, and modeling of the radial component of teleseismic P-waveforms. Conversely, to the south beneath the Tethyan Himalaya, no low-velocity zone was observed. The presence of the midcrustal low-velocity zone in the north implies that a partially molten layer is in the middle crust beneath the northern Yadong-Gulu rift and possibly much of southern Tibet." @default.
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- W2007751710 date "1996-12-06" @default.
- W2007751710 modified "2023-10-14" @default.
- W2007751710 title "Evidence from Earthquake Data for a Partially Molten Crustal Layer in Southern Tibet" @default.
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- W2007751710 doi "https://doi.org/10.1126/science.274.5293.1692" @default.
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