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.

Four assemblages of radiolaria found in the formation data the sequence from late Late Permian to early Middle Triassic,which greatly changes the generally estimated progress schedule for the Paleotethys evolution.

SmNd isotopic constraints on the age of the BangxiChenxing ophiolite in Hainan Island: implications for the tectonic evolution of eastern PaleoTethys.;

The Wilson Cycle of the Jinshajiang Paleo-Tethys Ocean, in Western Yunnan and Western Sichuan Provinces;

Triassic magmatism in the southern Lancangjiang zone,southwestern China and its constraints on the tectonic evolution of Paleo-Tethys

Paleomagnetic Constraints on the Closure Time of Paleo-Tethys:Implications for the Tectonic Setting of Formation of Triassic Songpan-Ganzi Flysch Complex

Lungmu Co-Shanghu plate suture in the Qinghai-Tibet Plateau and records of the evolution of the Paleo-Tethys Ocean in the Qiangtang area,Tibet,China;