A Historical Perspective on Ted Hughes Nature Poetry;

Regional fluid charecters and regimes of "Sanjiang" middle belt during Neo-Tethys.;

Deri′angma-Xiala section in the Xainza area, Tibet, China:A bridge for the stratigraphic and paleontological correlation between Gondwana and Tethys during the Late Carboniferous and Early Permian;

Relationship Among the Neo-Tethys,Tectonic Diktyogenises and Basins in West China;

It is regarded that paleo-Asian ocean and Tethyan ocean are the main factors controlling sedimentation and structure of the area, that structures.

The north slope area of the Mount Qomolangma being a main component of Tethyan Ocean belongs to Himalayan orogen intermediate on the junction between the northern India plate and Yarlung Zangbo river suture belt.

The study on the structure, volcanic sediment and magmatism shows that the east Kunlun Mountains belong to the Palaeo-Tethys active continental margin during the Hercynian-Indosinian period.