The solid-state nuclear track detectors have long been applied to assess the activity of tectonic faults. We measured the Radon (<em>Rn</em>) concentration in soil gas on 09 profiles with a total of 245 me...The solid-state nuclear track detectors have long been applied to assess the activity of tectonic faults. We measured the Radon (<em>Rn</em>) concentration in soil gas on 09 profiles with a total of 245 measurement points in Thua Thien Hue area (Vietnam). Measurement results show that the <em>Rn</em> concentration in soil gas ranges from ~10 Bq/m<sup>3</sup> to 144,570 Bq/m<sup>3</sup>. There is a clear difference in the <em>Rn</em> concentration on the granite rock of Dai Loc complex compared to the remaining rocks. The calculated background value and anomaly threshold of <em>Rn</em> concentration on the granite rock of Dai Loc complex and on the remaining rocks are 33,488 Bq/m<sup>3</sup>, 82,839 Bq/m<sup>3</sup> and 5313 Bq/m<sup>3</sup>, 24,850 Bq/m<sup>3</sup> respectively. Spatial distribution of Rn concentration in soil gas reflects the existence of faults since Rn concentration increases at the points above or near fault lines. The level of expression of fault activity is assessed by radon activity index (<em>KRn</em>), which is calculated by the ratio of anomaly value to background value of <em>Rn</em> concentration. According to <em>KRn</em>, in Thua Thien Hue area, only the Dakrong-Hue fault shows a strong expression of activity with high and very high <em>KRn</em> (the maximum <em>KRn</em> = 27.21). The Truong Son, Huu Trach River, Ta Trach River and Bo River fault zones do not show clear activity with low and medium <em>KRn</em>. There is no Rn anomaly value recorded on the Rao Trang fault, demonstrating that it is likely to be inactive at present. The study results indicate that the Rn concentration in soil gas is a strong evidence of the existence of faults or tectonic fracture zones as the <em>Rn</em> concentration always increases at the points above or near the fault line.展开更多
On August 8, 2017, a Ms 7.0 earthquake occurred 5 km to the west of Jiuzhaigou National Park, causing 25 deaths and injuring 525. The objective of this study was to explore the seismogenic fault of the earthquake and ...On August 8, 2017, a Ms 7.0 earthquake occurred 5 km to the west of Jiuzhaigou National Park, causing 25 deaths and injuring 525. The objective of this study was to explore the seismogenic fault of the earthquake and tectonic dynamics of the source rupture. Field investigations, radon activity tests, remote sensing interpretations, and geophysical data analyses were carried out immediately after the earthquake. The Jiuzhaigou earthquake occurred at the intersection of the northern margin of the Minshan uplift belt and the south part of the Wenxian–Maqin fault in the south margin of the West Qinling geosyncline. There are two surface rupture zones trending northwest(NW), which are ground coseismic ruptures caused by concealed earthquake faults. The rupture on the southwest is the structure triggering the earthquake, along the Jiuzhaitiantang–Epicenter–Wuhuahai. The other one on the northeast(Shangsizhai–Zhongcha–Bimang) is a reactivation and extension of the secondary fault trending NW. The source rupture of this earthquake is a strike-slipshear fracture associated with the fault plane trending NW 331° and steeply dipping 75°, which is continuously expanding at both ends. The tectonic dynamics process of the source rupture is that the "Jiuzhaigou protrusion" is left-lateral sheared along the seismogenic fault in the NW direction. Finally, the Maqin fault and the arc fault system at the top of the "Wenxian protrusion" will be gradually broken through sometime in far future, as well as earthquaketriggered landslides will be further occurred along the narrow corridor between the seismogenic faults. The research results revealed the basic geological data and tectonic dynamic mechanism in this earthquake.展开更多
文摘The solid-state nuclear track detectors have long been applied to assess the activity of tectonic faults. We measured the Radon (<em>Rn</em>) concentration in soil gas on 09 profiles with a total of 245 measurement points in Thua Thien Hue area (Vietnam). Measurement results show that the <em>Rn</em> concentration in soil gas ranges from ~10 Bq/m<sup>3</sup> to 144,570 Bq/m<sup>3</sup>. There is a clear difference in the <em>Rn</em> concentration on the granite rock of Dai Loc complex compared to the remaining rocks. The calculated background value and anomaly threshold of <em>Rn</em> concentration on the granite rock of Dai Loc complex and on the remaining rocks are 33,488 Bq/m<sup>3</sup>, 82,839 Bq/m<sup>3</sup> and 5313 Bq/m<sup>3</sup>, 24,850 Bq/m<sup>3</sup> respectively. Spatial distribution of Rn concentration in soil gas reflects the existence of faults since Rn concentration increases at the points above or near fault lines. The level of expression of fault activity is assessed by radon activity index (<em>KRn</em>), which is calculated by the ratio of anomaly value to background value of <em>Rn</em> concentration. According to <em>KRn</em>, in Thua Thien Hue area, only the Dakrong-Hue fault shows a strong expression of activity with high and very high <em>KRn</em> (the maximum <em>KRn</em> = 27.21). The Truong Son, Huu Trach River, Ta Trach River and Bo River fault zones do not show clear activity with low and medium <em>KRn</em>. There is no Rn anomaly value recorded on the Rao Trang fault, demonstrating that it is likely to be inactive at present. The study results indicate that the Rn concentration in soil gas is a strong evidence of the existence of faults or tectonic fracture zones as the <em>Rn</em> concentration always increases at the points above or near the fault line.
基金financially supported by the Open Research Fund from the Key Laboratory of Mountain Hazards and Earth Surface Process(Chinese Academy of Sciences)(Grant No.KLMHESP-17-06)the Independent Research Fund from the State Key Laboratory of Geohazard Prevention and Geoenvironment Protection(Chengdu University of Technology)(Grant No.40100-00002219)
文摘On August 8, 2017, a Ms 7.0 earthquake occurred 5 km to the west of Jiuzhaigou National Park, causing 25 deaths and injuring 525. The objective of this study was to explore the seismogenic fault of the earthquake and tectonic dynamics of the source rupture. Field investigations, radon activity tests, remote sensing interpretations, and geophysical data analyses were carried out immediately after the earthquake. The Jiuzhaigou earthquake occurred at the intersection of the northern margin of the Minshan uplift belt and the south part of the Wenxian–Maqin fault in the south margin of the West Qinling geosyncline. There are two surface rupture zones trending northwest(NW), which are ground coseismic ruptures caused by concealed earthquake faults. The rupture on the southwest is the structure triggering the earthquake, along the Jiuzhaitiantang–Epicenter–Wuhuahai. The other one on the northeast(Shangsizhai–Zhongcha–Bimang) is a reactivation and extension of the secondary fault trending NW. The source rupture of this earthquake is a strike-slipshear fracture associated with the fault plane trending NW 331° and steeply dipping 75°, which is continuously expanding at both ends. The tectonic dynamics process of the source rupture is that the "Jiuzhaigou protrusion" is left-lateral sheared along the seismogenic fault in the NW direction. Finally, the Maqin fault and the arc fault system at the top of the "Wenxian protrusion" will be gradually broken through sometime in far future, as well as earthquaketriggered landslides will be further occurred along the narrow corridor between the seismogenic faults. The research results revealed the basic geological data and tectonic dynamic mechanism in this earthquake.
