In the exploration of the hidden Haihe fault,radon and mercury in soil gas were measured by using FG-3017 radon detector and XG-4 mercury analyzer.In this paper,based on the measurement results of 12 fault gas profile...In the exploration of the hidden Haihe fault,radon and mercury in soil gas were measured by using FG-3017 radon detector and XG-4 mercury analyzer.In this paper,based on the measurement results of 12 fault gas profiles,and integrating with the exploration results of artificial seismic prospecting,the relationship between anomalous site of fault gas and fault location is analyzed.Using the relationship between anomalous strength of fault gas and fault activity,the activity of Haihe fault is studied,thus the location and activity segmentation of the Haihe fault in Tianjin region are presented.This study shows that the method of fault gas detection can not only identify the preliminary location of fault,but also make preliminary segmentation of fault activity.The fault detected by the method of fault gas measurement is shown as a band.Through contrasting with exploration results of artificial seismic prospecting and analyzing,we find that the fault is located inside the band.According to the measurements of soil gas radon,the Haihe fault can be divided into east and west segments and the activity of the east segment of Haihe fault is stronger than that of the west segment.This is only a relative result,and it is difficult to judge whether the fault is active or not with this result.展开更多
Structural characteristics of the Jurassic basins of Xining, Minhe, and Xiji in the east of middle Qilian were researched based on the data obtained by gravitational, magnetic, and seismic methods. The result shows th...Structural characteristics of the Jurassic basins of Xining, Minhe, and Xiji in the east of middle Qilian were researched based on the data obtained by gravitational, magnetic, and seismic methods. The result shows that each of these three basins is an independent structural unit with a NW strike and being separated by upheavals. Two groups of faults with NW and NE directions are developed in the basin, which controls the formation and evolution of the (Jurassic basins). The NW faults are the main ones while the NE faults are the secondary for controlling the sedimentation. Of the three basins, the Minhe basin is the favorable prospecting area.展开更多
基金This research was sponsored by the project of Quantitative Evaluation of Activity of the Hidden Haihe Fault in Tianjin City (Grant No. JINJI290)
文摘In the exploration of the hidden Haihe fault,radon and mercury in soil gas were measured by using FG-3017 radon detector and XG-4 mercury analyzer.In this paper,based on the measurement results of 12 fault gas profiles,and integrating with the exploration results of artificial seismic prospecting,the relationship between anomalous site of fault gas and fault location is analyzed.Using the relationship between anomalous strength of fault gas and fault activity,the activity of Haihe fault is studied,thus the location and activity segmentation of the Haihe fault in Tianjin region are presented.This study shows that the method of fault gas detection can not only identify the preliminary location of fault,but also make preliminary segmentation of fault activity.The fault detected by the method of fault gas measurement is shown as a band.Through contrasting with exploration results of artificial seismic prospecting and analyzing,we find that the fault is located inside the band.According to the measurements of soil gas radon,the Haihe fault can be divided into east and west segments and the activity of the east segment of Haihe fault is stronger than that of the west segment.This is only a relative result,and it is difficult to judge whether the fault is active or not with this result.
文摘Structural characteristics of the Jurassic basins of Xining, Minhe, and Xiji in the east of middle Qilian were researched based on the data obtained by gravitational, magnetic, and seismic methods. The result shows that each of these three basins is an independent structural unit with a NW strike and being separated by upheavals. Two groups of faults with NW and NE directions are developed in the basin, which controls the formation and evolution of the (Jurassic basins). The NW faults are the main ones while the NE faults are the secondary for controlling the sedimentation. Of the three basins, the Minhe basin is the favorable prospecting area.
