In this paper,the authors have mainly summarized three seismic detection methods for revealing the Moho depth of the Qinghai-Tibet plateau based on previous achievements.

In this paper,the authors have summarized the results of deep seismic sounding,deep seismic profiling and broadband seismic observation and dealt with the variation features of the Moho depth.

Moho Depths Inversion of Qinghai-Tibet Plateau with Variable Density Model;

The Study on the fluctuation of Moho in Yellow Sea and its adjacent area;

It is confirmed that Jiyang depression of Paleogene occurred in trans-extensional behavior in the light of Moho uplifting,lithosphere thinning,development of basic and ultra basic igneous rocks in mantle source rocks,high geothermal gradient,halfgraben-like depression bas.

Airry isostatic anomalies and Moho-depth were calculated and analysed.

Subtracting the gravity anomalies caused by density anomalies from the observed Bouguer anomalies, we inversed the depth of Moho of northwestern China by using the residu- al anomalies.

A Review on the Moho Discontinuity beneath the Tibetan Plateau;

The infrastructure of this zone is apparently controlled by the transitional belt between the mantle slope of Yunyang backbone and the mantle flat of Xunyang on Moho discontinuity and by the western marginal rim of Wudang platform on Conrad discontinuity.

Some new viewpoints were proposed concerning the trend and extension of the southwestern end of the Altun strike-slip fault,the origin of two low gravity zones was discussed,the altitude of the Moho discontinuity in the .