is the main peak of the Longmen Mountains, where the famous fault line occurs from southwest to northeast, while very rich biodiversity is found and several nature reserves are located in this region.

α Diversity of Communities and Their Changes Along Altitude Gradient in the Baishuihe National Nature Reserve on the Longmen Mountains, Sichuan;

Structural analysis of Kuangshanliang in the northern Longmenshan fold-thrust belt and its hydrocarbon exploration;

Karst Features and Genesis of Gexianshan Carbonate Allochthon in Tabgbazi,Longmenshan(Continued);

Tourism resources of the National Longmenshan Geopark and its developmental strategy;

Remote sensing investigation and assessment of tourism resources in the south of Longmen mountain (Lushan Area);

Correlations between vegetation distribution and topographical factors in the northwest of Longmen Mountain,Sichuan Province.;

The fluid inclusions and stable isotope geochemistry are adopted to study the fluid characteristics and to reveal the path of fluid migration in the West Sichuan Foreland Basin the Longmen Mountain transition .

The Features and Measures of Mountain Hazards Triggered by Earthquake in Longmenshan Mountains;

The Longmenshan Mountains area is one of major metallogenic provinces(belts) in Sichuan.

A primary analysis of geophysical and geodynamic features of the Wenchuan earthquake in Longmen Mountains,Sichuan,China;

Structural features of the central Longmen Mountains and the Wenchuan earthquake in Sichuan,China;

The large-scale gliding-type klippe system in Longmen Mountains and neotectonic activity of the Longmen Orogen;

In the paper, the author proposes that there are four steps to determine the primitive postion for nappes by researching Devonian in the middle northern Fore Longmenshan area.