By analyzing the seismic mechanism of the Tangshan earthquake and its pattern of movement through the study of ground deformation and ground strain of the Tangshan earthquake area it is clear that the breeding and occurrence of this event are controlled by a long-term intense active fault zone. By the ground deformation, displacement, tectonic features and seismic effects after the event, this causative fault is known to be composed of a group of NNE trending right turn strike-slip faults and thus we call it the Tangshan active fault zone
The focal mechanism solutions of the M5. 1 Badong earthquake and subsequent 34 aftershocks at ML 2. ...
The Xianshuihe fault is one of the most active faults in southwestern China. Recently, three large e...
The Huaxian magnitude 8 great earthquake of January 23, 1556, is the largest one recorded in the Wei...
The mechanism and reoccurrence rule of surface faulting have been analyzed based on macroscopic insp...
The intensive ground movement of seismic region was an essential factor in causing ground damages. D...
The geodynamics and faulting mechanism of the M7.8 Tangshan earthquake (China, 28th July 1976) are r...
This paper describes the significant settlement of buildings on saturated soft clay due to Tangshan ...
The Tangshan earthquake (M_s = 7.7), of July 27, 1976 and its principal aftershock (M_s = 7.2), whic...
No other earthquake in the 20th or 21st centuries was as catastrophic or claimed as many lives as th...
The city of Tangshan lies on the edge of the North China Plain, south of the Yanshan mountain range ...
Georesistivity precursors and corresponding coseismic effects to the Tangshan earthquake of 1976 are...
Space-and-time regularities of seismicity of the North China (Tan-Lu) zone are studies, and tectonic...
On November 14, 2001, a great earthquake with a magnitude of Ms=8.1 occurred in the Qinhai-Tibet Pla...
The special geological conditions in the Xiji-Langfu area are the main reason for the anomalous high...
The Xianshuihe fault is an important strike - slip and strong seismogenic zone in West China. The ac...
The focal mechanism solutions of the M5. 1 Badong earthquake and subsequent 34 aftershocks at ML 2. ...
The Xianshuihe fault is one of the most active faults in southwestern China. Recently, three large e...
The Huaxian magnitude 8 great earthquake of January 23, 1556, is the largest one recorded in the Wei...
The mechanism and reoccurrence rule of surface faulting have been analyzed based on macroscopic insp...
The intensive ground movement of seismic region was an essential factor in causing ground damages. D...
The geodynamics and faulting mechanism of the M7.8 Tangshan earthquake (China, 28th July 1976) are r...
This paper describes the significant settlement of buildings on saturated soft clay due to Tangshan ...
The Tangshan earthquake (M_s = 7.7), of July 27, 1976 and its principal aftershock (M_s = 7.2), whic...
No other earthquake in the 20th or 21st centuries was as catastrophic or claimed as many lives as th...
The city of Tangshan lies on the edge of the North China Plain, south of the Yanshan mountain range ...
Georesistivity precursors and corresponding coseismic effects to the Tangshan earthquake of 1976 are...
Space-and-time regularities of seismicity of the North China (Tan-Lu) zone are studies, and tectonic...
On November 14, 2001, a great earthquake with a magnitude of Ms=8.1 occurred in the Qinhai-Tibet Pla...
The special geological conditions in the Xiji-Langfu area are the main reason for the anomalous high...
The Xianshuihe fault is an important strike - slip and strong seismogenic zone in West China. The ac...
The focal mechanism solutions of the M5. 1 Badong earthquake and subsequent 34 aftershocks at ML 2. ...
The Xianshuihe fault is one of the most active faults in southwestern China. Recently, three large e...
The Huaxian magnitude 8 great earthquake of January 23, 1556, is the largest one recorded in the Wei...