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 .

Based on the comparative analysis and study on 10 profiles of telluric electromagnetic sounding (MT) and regional gravimetric,magnetic data and Moho surface,the deep geological tectonic pattern of the central southern Jiangxi is discussed in this paper.

Using the formulae, data of gravity measurement and leveling survey in the Hexi region of Gansu province and northwestern Yunnan province are computed, for study on variations of the lower crustal interface density and vertical deformation of Moho surface with time.

Moho depth and sedimentary thickness in Capital region;

In this paper, we use the teleseismic receiver function to determine the Moho depth and the one dimension velocity model under Xi′an Seismic Station.

The obtained Moho depth,crustal structure thickness,and Cenozoic and Mesozoic basement show that the formation mechanism of Mesozoic basins is different from that of the Cenozoic basins.