[1] Du J G, Si X Y, Chen Y X, et al. Geochemical anomalies connected with great earthquakes in China. Geochemistry Research Advances[J]. Geochemistry Research Advances, 2008, 1-37. [2] 李营, 杜建国, 王富宽, 等. 延怀盆地土壤气体地球化学特征[J]. 地震学报, 2009, 31(1): 82-91. [3] Zhou X C, Du J G, Chen Z, et al. Geochemistry of soil gas in the seismic fault zone produced by the Wenchuan MS8. 0 earthquake, southwestern China[J]. Geochemical Transactions, 2010, 11: 5. [4] 冉勇康. 我国几个典型地点的古地震细研究和大地震重复行为探讨[D]. 北京: 国家地震局地质研究所, 1997. [5] 谢富仁, 张红艳, 崔效峰, 等. 延怀盆地活动断裂运动与现代构造应力场[J]. 地震地质, 2007, 29(4): 693-705. [6] 周晓成, 王传远, 柴炽章, 等. 海原断裂带东南段土壤气体地球化学特征[J]. 地震地质, 2011, 33(1): 123-132. [7] Ciotoli G, Lombardi S, Annunziatellis A: Geostatistical analysis of soil gas data in a high seismic intermontane basin: Fucino Plain, central Italy. Journal of Geophysical Research 2007, 112: 23, B05407. [8] Al-Hilal M, Al-Ali A. The role of soil gas radon survey in exploring unknown subsurface faults at Afamia B dam, Syria[J]. Radiation Measurements, 2010, 45: 219-224. [9] Sugisaki R. Behavior and origin of helium, neon, argon and nitrogen from active faults[J]. J. Geophys. Res., 1987, 92: 12523-12530. [10] 韩晓昆. 首都圈地震重点监测区土壤气体地球化学[D]. 北京: 中国地震局地震预测研究所, 2014. [11] 周晓成, 柴炽章, 雷启云, 等. 银川隐伏断层带土壤气中H2的地球化学特征[J]. 物探与化探, 2013, 37(1): 147-149. [12] Chiodini G, Caliro S, Cardellini C, et al. Carbon isotopic composition of soil CO2 efflux, a powerful method to discriminate different sources feeding soil CO2 degassing in volcanic-hydrothermal areas[J]. Earth and Planetary Science Letters, 2008, 274(3-4): 372-379. [13] Lewicki J L, Evans W C, Hilley G E, et al. Shallow soil CO2 flow along the San Andreas and Calaveras Faults, California[J]. J. Geophys. Res., 2003, 108(B4): 2187. [14] 车用太. 地下流体数字观测技术[M]. 北京: 地震出版社, 2002, 1-120. [15] Weinlich F H, et al. Fault delineation study using soil-gas method in the Dharamsala area, NW Himalayas, India[J]. Radiation Measurements, 2008, 43: S337-S342. [16] Wang G, Zhang Z, Wang M. Implications of ground water chemistry and flow patterns for earthquake studies[J]. Ground Water, 2005, 43: 478-484. [17] Li Y, Du J, Wang X, et al. Spatial variations of soil gas geochemistry in the Tangshan area of Northern China[J]. Terr. Atmos. Ocean. Sci., 2013, 24: 323-332, doi: 10. 3319/TAO. 2012. 11. 26. 01(TT). Spatial Variations of Soil Gas Geochemistry in the Tangshan Area of Northern China [18] 赵振燊. 甘东南地震重点危险区主要活动断裂带断层气地球化学特征[D]. 兰州: 中国地震局兰州地震研究所, 2012. [19] Vivek Walia, Lin S J, Hong W L. Continuous temporal soil-gas composition variations for earthquake precursory studies along Hsincheng and Hsinhua faults in Taiwan[J]. Radiation Measurements, 2009, 44: 934-939. [20] Ma M, Wang D, Sun R, et al. Gaseous mercury emissions from subtropical forested and open field soils in a national nature reserve, southwest China[J]. Atmospheric Environment, 2013, 64: 116-123. [21] 韩孔艳. 张家口—渤海构造带的分段性与地震活动特征研究[D]. 北京: 中国地震局地质研究所, 硕士研究学位论文, 2009. [22] 杨博, 占伟, 刘志广. 晋冀蒙交界区水平向构造活动的基本特征及动态变化[J]. 地震研究, 2013, 36(4): 472-477. |