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- W2364526156 abstract "A 3-D lithospheric structure of P-wave velocity in the Sulu -Dabie orogen area has been studied based on the results from the Global Geological Transect projects (GGT), wide-angle seismic sounding, teleseismic tomography and other data. The obtained results are shown in plates with the data density of 1°×1°. The lithospheric structures in the ultra-high pressure metamorphic (UHPM) belts in the Sulu and Dabie areas show similar characteristics more or less. Higher P-wave velocity exists in the upper crust and forms a convex high-velocity region. The thicken middle crust is characterized by normal or lower P-wave velocity. The Moho discontinuity is depressed under the UHPM terranes. The Moho discontinuity in the Sulu and Dabie orogen areas are deeper than their surroundings and the depths reach 32~33 km and 34~38 km, respectively. The P-wave velocity of the upper crust in the Sulu UHPM belt is higher than that in the Dabie area. The depressing of the Moho discontinuity beneath the Dabie, however, is obviously deeper than that beneath the Sulu region. It is attributable to the effect of the left-lateral strike-slip movement along the Tanlu fault in the Sulu area." @default.
- W2364526156 created "2016-06-24" @default.
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- W2364526156 date "2003-01-01" @default.
- W2364526156 modified "2023-09-26" @default.
- W2364526156 title "Three-dimensional Velocity Structures of the Sulu -Dabie Orogen Belt" @default.
- W2364526156 hasPublicationYear "2003" @default.
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