(1) Institute of Geophysics, State Seismological Bureau, 100081 Beijing, China;(2) Institute of Geodynamics, State Seismological Bureau, 100085 Beijing, China
Abstract:
The shear-wave splitting was analyzed on the deep seismic sounding profile crossing the Dabieshan area. The direction difference
between Sg and SmS fast wave polarization indicates that the modem regional tectonic stress field in the Dabieshan area exists
only in uppcr crust, while the crack alignment caused by the Triassic collision between the North China and the Yangtze blocks
had been preserved in mid-lower curst.