The stability of Shule River fault zone is mainly dominated by the neotec-tonic movement pattern and strength of its two sid.

On the basis of characteristics of remote sensing interpretation in the middle region of Shule River fault zone and its north Beishan area,stability evaluations on the construction of Beishan rock mass have been made by analyzing characteristics of gravity,seismicity,stress state of active fault and seismogenic mechanical condition.

Based on remote-sensing geology and very-low frequency anomalies of the central part of the Shule River fault zone, this paper,by means of determining concentration of radon emanation at the surface above the fault zone, has analysed and evaluated the stability of the central part of the Shule River fault zone.

Study on fractal characteristic of hydrographic nets and activity of the Red River Fault Zone;

The Red River Fault Zone is a gigantic sliding fault zone beginning from the east of Qinzang plateau in the north to the northwest of Yunnan, and passing through the north of Vietnam, and then extending to South China Sea, the whole length is over 1000km.

The Red River Fault Zone is a large slide and active fault zone.

Geophysical research on deep structure feature in study region of red river fault zone;

We used double difference location method to relocate the moderate-small earthquakes on the Red River fault zone of Yunnan from 1999 to 2003, and analyzed the relationship of relocation result and geologic structure.

The Red River Fault Zone is a strike-slip zone along which Indochina Block was extruded during India-Tibet collision.