Zhi Guo

Midcrustal low-velocity layer beneath the central Himalaya and southern Tibet revealed by ambient noise array tomography

Lower-crust S-wave velocity beneath western Yunnan Province from waveform inversion of dense seismic observations

A study of the velocity structure beneath Himalaya mountain chain region using transform function method

Depth variations of azimuthal anisotropy beneath the Tian Shan Mt range (NW China) from ambient noise tomography

S-wave velocity of the crust around Tianshan Mountains inverted from seismic ambient noise tomography

Crustal structure beneath the central Tien Shan from ambient noise tomography

Midcrustal low-velocity layer beneath the central Himalaya and southern Tibet revealed by ambient noise array tomography: LOW-VELOCITY LAYER BENEATH SOUTHERN TIBET

Crustal and uppermost mantle structures of the South China from joint analysis of receiver functions and Rayleigh wave dispersions

Rupture process of the Oct. 6, 2008 M(s)6.6 Damxung earthquake, Tibet, China

Crust structure beneath Tengehong-Lincang region, Yunnan province, revealed by transform function