Altun foothill belt of western Qaidam basin is regarded as a major pre-exploration belt with abundant petroleum resources, high geological evaluation, low explorative degree and great potentials for prospecting.

The inversion for the Q value of the upper crust along the profile from Baicheng to Da Qaidam has been carried out using seismic reflection/refraction data acquired on the profiles which cross the Tarim basin, the Altun orogenic belt and the Qaidam basin, respectively.

Mesozoic paleocurrent properties in the southern edge of Altyn Mountain in the western Qaidam Basin;

Tectonic Attribution and Movement Characteristic of Altyn Mountain;

Advance in study of Mesozoic-Cenozoic uplift history of the Altyn Mountains;

Early Paleozoic Magmatism and Gold Metallogenesis in Altun Mountains, Northwest China;

Sedimentary geochemistry and significance of the Middle and Lower Jurassic strata in the frontal areas of the Altun Mountains,Qinghai;

Lower-middle Jurassic distribution and oil-gas exploration direction on the southern Altyn tagh in the western Qaidam Basin;

Geothermochronology and tectonic evolution of Eastern Altyn Tagh Mountains,Northwestern China

It is concluded that the different order structures in Altyn Tagh fault system controlled the spatial distribution of metallogenic belts,ore fields and ore deposits.

Available surface water resources and potential of water development in the Altun mountains and the Qiangtang Plateau;

Three alkali-rich intrusive rock belts in Kunlun Mountain and Altun Mountain area;

Structural Features of the Altun Mountain and Its Fault Systems During Mesozoic and Cenozoic;