Abstract
The studies of seismic tomography and wide-angle reflection have been carried out to reveal the velocity structure beneath the eastern Dabie orogenic belt. The result from the seismic tomography shows the high velocity bodies might be positioned to a depth of only about 1.5 km below sea level within the Dabie ultra-high pressure metamorphic (UHPM) belt; the fan-profile shows the Shuihou-Wuhe fault, the demarcation between the South Dabie and the North Dabie, slopes to the south-west at a dip angle of about 45° in the bottom of upper crust. The wide-angle reflection shows the middle crustal boundaries and the complex features from the lower crust.
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