汶川MS8.0地震前四川地区前兆异常及其统计分析

程万正官致君 苏 琴 阮 祥 张致伟

程万正官致君 苏 琴 阮 祥 张致伟. 2011: 汶川MS8.0地震前四川地区前兆异常及其统计分析. 地震学报, 33(3): 304-318.
引用本文: 程万正官致君 苏 琴 阮 祥 张致伟. 2011: 汶川MS8.0地震前四川地区前兆异常及其统计分析. 地震学报, 33(3): 304-318.
Cheng Wanzheng Guan Zhijun Su Qin Ruan Xiang Zhang Zhiweiaylc. 2011: Precursory anomalies inSichuanregion before 2008 Wenchuan MS8.0 earthquake and their statistical analysis. Acta Seismologica Sinica, 33(3): 304-318.
Citation: Cheng Wanzheng Guan Zhijun Su Qin Ruan Xiang Zhang Zhiweiaylc. 2011: Precursory anomalies inSichuanregion before 2008 Wenchuan MS8.0 earthquake and their statistical analysis. Acta Seismologica Sinica, 33(3): 304-318.

汶川MS8.0地震前四川地区前兆异常及其统计分析

详细信息
  • 中图分类号: P315.63

Precursory anomalies inSichuanregion before 2008 Wenchuan MS8.0 earthquake and their statistical analysis

  • 摘要: 研究了2008年5月12日汶川MS8.0地震前四川地区观测到的各种异常.异常项与所有测项(或测站、台、场地、井点、泉点)之比称为异常测项(测点)比,以下类同. 地震前四川地区流动短水准观测存在中长期趋势异常的场地比为0.28,异常测项比为0.20;流动短基线存在中期趋势异常的场地比为0.13,异常测项比为0.13;地倾斜类观测存在中期趋势异常的台站比0.17,异常测项比为0.13;地下水位观测存在中期趋势异常的水位井点比为0.20;温泉观测存在水温短期异常的泉点比为0.15;温泉水氡、气氡观测存在短期异常的台点比为0.08,异常测项比为0.04;井泉水质组分观测存在短期异常的台点比为0.20,异常测项比为0.04;视电阻率观测存在中期异常的台站比为0.17, 异常测项比为0.06.对同一观测台或场地有不同观测手段,分别计算了台或场地数:四川地区在汶川8.0级地震前各类观测台或场地共有172个,存在观测异常台或场地比为0.14,其中出现中期与短期异常场地比分别是0.08和0.03;各类观测项共有335项,异常测项比为0.09,其中出现中期与短期异常测项的占比分别是0.06和0.01.可见,震前仪器微观监测台或测项多数没有观测到突出异常现象.本文中其它没有提及的观测手段或观测项的资料,经过研究没有分析检测出异常项.
    Abstract: Various observation anomalies in Sichuan region before the 12 May 2008 Wenchuan MS8.0 earthquake were studied. The abnormal items against all of observation items (or observation stations, measuring platforms, sites, well points, spring points) are the ratio of abnormal items (points), following are similar. On the mobile short leveling, the site and item ratios of existing medium to long-erm trend anomalies are 0.28 and 0.20 respectively. On the mobile short baseline, the site and item ratios of existing medium-erm trend anomalies are 0.13 and 0.13 respectively. On the ground tilt measurement, the station ratio of medium-erm trend anomalies is 0.17, the abnormal item ratio is 0.13. On the groundwater level observation, the well point ratio of medium-erm trend anomalies is 0.20. On the hot spring observation, the spring point ratio of short-erm anomalies is 0.15. On the hot spring water-as radon observation, the station and point ratio of short-erm anomalies is 0.08, the abnormal item ratio is 0.04. On the well water quality component observation, the station and point ratio of short-erm anomalies is 0.02, the abnormal item ratio is 0.04. On the apparent resistivity, the station and items ratios of medium-erm anomalies are 0.17 and 0.06 respectively. There have various observation means in the same station or site, we calculate the station or site number. There are 172 various stations or sites in Sichuan area before the Wenchuan MS8.0 earthquake, and abnormal stations or sites ratio is 0.14, the site ratios of appearing medium-erm and short-erm anomalies are 0.08 and 0.03 respectively. The total of various observation items are 335, the ratio of abnormal items is 0.09. The ratios of medium-erm and short-erm abnormal items are 0.06 and 0.01 respectively. It is clear that there are not obvious anomalies recorded by station or observation items before the earthquake. As for other observation means and data of observation items which are not involved in this paper, after researching, there have no abnormal items.
  • 期刊类型引用(15)

    1. 芮雪莲,杨耀,龙锋,赵敏,官致君. 四川乡城然乌温泉水文地球化学特征和成因分析. 地震. 2024(03): 173-195 . 百度学术
    2. 孟宪森. 地震预测工作的几个问题讨论. 地震地磁观测与研究. 2023(S1): 271-273 . 百度学术
    3. 王晓涛,马禾青,崔瑾,李国斌,丁风和. 汶川8.0级地震宁夏前兆异常回顾与同震响应特征分析. 地震工程学报. 2022(01): 192-202 . 百度学术
    4. Chenglong Liu,Guangcai Wang,Zheming Shi,Dan Zhao,Hui Zhang. Possible precursory anomalies in ground water level associated with the Wenchuan Ms 8.0 earthquake in 2008, Sichuan, China. Geodesy and Geodynamics. 2020(02): 127-134 . 必应学术
    5. ZHAO Jing,LIU Jie,REN Jinwei,YUE Chong,LI Jiaojiao. Deformation Evolution Characteristics Revealed by GPS and Cross-fault Leveling Data before the M_S8. 0 Wenchuan Earthquake. Earthquake Research in China. 2019(03): 461-477 . 必应学术
    6. 张小涛,刘杰,宋治平,薛艳,张永仙,晏锐,苑争一. 汶川M_S8.0地震的前兆异常时空演化过程及其力学分析. 地震. 2018(02): 72-83 . 百度学术
    7. 晏锐,田雷,王广才,钟骏,刘杰,周志华. 2008年汶川8.0级地震前地下流体异常回顾与统计特征分析. 地球物理学报. 2018(05): 1907-1921 . 百度学术
    8. Zhang Xiaotao,Liu Jie,Song Zhiping,Xue Yan,Zhang Yongxian,Yan Rui,Yuan Zhengyi. Temporal and Spatial Evolution of Precursory Anomalies of the Wenchuan M_S8.0 Earthquake and Their Mechanical Analysis. Earthquake Research in China. 2018(02): 212-226 . 必应学术
    9. 赵静,刘杰,任金卫,江在森,闫伟,岳冲,苑争一. 汶川8.0级地震前GPS与跨断层资料反映的运动与变形演化特征. 中国地震. 2018(03): 414-427 . 百度学术
    10. 邱桂兰. 芦山M7.0级与汶川M8.0级地震前兆异常对比. 四川地震. 2015(01): 14-20 . 百度学术
    11. 路茜,张铁宝,辛华,刘放. 汶川8.0级和芦山7.0级地震前卫星热红外异常现象对比. 四川地震. 2014(02): 38-42 . 百度学术
    12. 郭国祥,张红秀,郭林旺,刘国俊,邰垣东. 山西临汾中心地震台数字化定点形变观测异常与地震对应关系分析. 山西地震. 2014(02): 21-24 . 百度学术
    13. 万文妮. 山西带断层形变特征研究. 地震. 2012(02): 145-153 . 百度学术
    14. 程万正,刁桂苓. 从汶川和日本巨震浅论我国地震预测的可应用性问题. 国际地震动态. 2012(10): 23-29 . 百度学术
    15. Abnormal interruption of water flow from an artesian well prior to 2008 Wenchuan earthquake. Geodesy and Geodynamics. 2011(02): 53-57 . 必应学术

    其他类型引用(5)

计量
  • 文章访问数:  2104
  • HTML全文浏览量:  567
  • PDF下载量:  220
  • 被引次数: 20
出版历程
  • 发布日期:  2011-05-19

目录

    /

    返回文章
    返回