New understanding on origin of Kalaxiangeer copper deposit on southern margin of Altay mountain, Xinjiang: Constraints from S-Pb-H-O isotope geochemistry and ~(40)Ar-~(39)Ar age of Halasu copper deposit;

Geology and Metallogenic Model of the Altay Large Metallogenic Belt in Kazakhstan;

Classification and Exploration Indication of the Gold Deposit in Altay,Xinjiang,China;

Volcanic sedimentary structure evolvement and mineralization of Mengku basin at south margin of Altai mountain,Xinjiang;

Ages and origin of the early Devonian granites from the north part of Chinese Altai Mountains and its tectonic implications.;

Geochemical characteristics and ~(40)Ar-~(39)Ar ages of the amphibolites and gabbros in Tarlang area:implications for tectonic evolution of the Chinese Altai.;

Fission track evidences for tectonic activity in Altay Mountains, Xinjiang, North-Western China;

Oxygen Isotope Exchange Kinetics between Coexistent Minerals and Water in Some Granite Plutons of the Altay Mountains;

Discovery of the Kumasu gold polymetallic deposit in the Nurt area, Altay Mountains, and ore prospect evaluation;

REE geochemistry of Qiaoxiahala type Fe-Cu deposits in southern margin of Altay Mountains, Xinjiang, and its geological implications;

Metal logeny of Polymetallic Metal logenic Belts on the Southern Margin of the Altay Mountains, Xinjiang,China;

The composition of flora is a young one with little ancient characters which was formedgradually during the uplifting of the Altai Mountain, at the same time, it has fragile character.

The Jintas Steppe Grassland Nature Reserve with an elevation between1000 and 3000m is situated in the middle section of South Altai Mountain.

Research and Protection on Sanger, Altai Falcon and Gyrfalcon;