Characteristics of the correlation coefficient of spectral amplitude of earthquake sequences in western Yunnan region since 2008
-
摘要: 使用云南数字地震台网记录的波形数据, 计算了滇西地区2008—2011年发生的6个MS≥4.0地震序列的谱振幅相关系数. 结果表明, 这些地震序列无论是前震型、 主震-余震型, 还是震群型地震, 其谱振幅相关系数均较高, 分析认为可能是该区域处于高应力水平状态所造成的. 谱振幅相关系数较小的地震序列, 其震源机制一致性不高, 区域应力场强度较低, 可以作为判别后续没有更大地震的指标. 前震序列的谱振幅相关系数较高, 但谱振幅相关系数较高的不一定是前震序列. 地震序列的谱振幅相关系数较高, 仅仅表明其区域应力水平较高, 这种状态有利于该区域MS≥5.0地震的再次发生.Abstract: Using digital seismic waves recorded by Yunnan Digital Seismic Network, we calculated the correlation coefficient of spectral amplitude of six MS≥4.0 earthquake sequences occurred from 2008 to 2011 in western Yunnan region. The results suggest that the correlation coefficient of spectral amplitude of earthquake sequences are generally high value, no matter the sequence is foreshock, main shock-aftershock or earthquake swarm, which may be caused by high stress filed in the source region. A smaller correlation coefficient of spectral amplitude, which means less consistency of focal mechanisms and low level of stress filed, can be used as an index to predict that larger earthquakes will not follow behind. The correlation coefficient of spectral amplitude of foreshock sequence is larger; however, a larger correlation coefficient does not indicate the earthquake sequence is foreshock. A larger correlation coefficient of spectral amplitude only implies high level of the stress field, but it is beneficial to occurring MS≥5.0 earthquake in the source region.
-
-
图 1 畹町台(WaD)记录到的一次地震的波形(a)及计算得到的相应观测位移谱(b)
Z, T和R分别表示垂向、 切向和径向分量; PZ和PR分别表示P波位移谱的垂向和 径向分量; SZ, SR和ST分别表示S波位移谱的垂向、 径向和切向分量
Figure 1. Waveform of one earthquake recorded by the station WaD (a), and corresponding displacement spectra from observed data (b)
Z, T and R represent vertical, tangential and radial components, respectively. PZ and PR represent vertical and radial components of the P-wave displacement spectrum, respectively. SZ, SR and ST represent vertical, radial and tangential components of the S-wave displacement spectrum, respectively
图 2 滇西地区地震序列和台站(三角形表示)分布
① 2008-03-21盈江MS5.2地震序列; ② 2008-08-20和08-21盈江MS4.9,MS5.8地震序列; ③ 2010-04-02和04-03腾冲MS4.3,MS4.0地震序列; ④ 2010-06-01施甸MS4.8地震序列; ⑤ 2011-03-10盈江MS5.8地震序列; ⑥ 2011-06-20和08-09腾冲MS5.3,MS5.2地震
Figure 2. Distributions of earthquake sequences and stations (denoted by solid triangles) in western Yunnan region
① MS5.2 Yingjiang earthquake sequence of March 21,2008; ② MS4.9 and MS5.8 Yingjiang earthquake sequence of August 20,2008 and August 21,2008,respectively; ③ MS4.3 and MS4.0 Tengchong earthquake sequence of April 2,2010 and April 3,2010,respectively; ④ MS4.8 Shidian earthquake sequence of June 1,2010; ⑤ MS5.8 Yingjiang earthquake sequence of March 10,2011; ⑥ MS5.3 and MS5.2 Tengchong earthquake sequence of June 20,2011 and August 9,2011,respectively
图 3 滇西地区6个地震序列的震级-时间及相关系数图
(a)2008-03-21盈江MS5.2地震序列;(b)2008-08-20和08-21盈江MS4.9,MS5.8地震序列; (c)2010-04-02和04-03腾冲MS4.3,MS4.0地震序列;(d)2010-06-01施甸MS4.8地震序列; (e)2011-03-10盈江MS5.8地震序列;(f)2011-06-20和08-09腾冲MS5.3,MS5.2地震序列
Figure 3. M -t plots and the correlation coefficient of spectral amplitude of six earthquake sequences in western Yunnan region
(a)MS5.2 Yingjiang earthquake sequence of March 21,2008;(b)MS4.9 and MS5.8 Yingjiang earthquake sequence of August 20,2008 and August 21,2008,respectively;(c)MS4.3 and MS4.0 Tengchong earthquake sequence of April 2,2010 and April 3,2010,respectively;(d)MS4.8 Shidian earthquake sequence of June 1,2010; (e)MS5.8 Yingjiang earthquake sequence of March 10,2011;(f)MS5.3 and MS5.2 Tengchong earthquake sequence of June 20,2011 and August 9,2011,respectively
表 1 2008年以来滇西地区部分MS≥4.0地震的基本参数
Table 1 Basic parameters of partial MS≥4.0 earthquakes in western Yunnan region since 2008
表 2 地震序列的谱振幅相关系数及类型统计
Table 2 Statistics on the correlation coefficient of spectral amplitude and types of earthquake sequences
-
陈颙. 1978. 用震源机制一致性作为描述地震活动性的新参数[J]. 地球物理学报, 21(2): 142-159. Chen Y. 1978. Consistency of focal mechanism as a new parameter in describing seismic activity[J]. Acta Geophysica Sinica, 21(2): 142-159 (in Chinese).
崔子健, 李志雄, 陈章立, 赵翠萍, 郑斯华, 周连庆. 2012. 判别小震群序列类型的新方法研究: 谱振幅相关分析法[J]. 地球物理学报, 55(5): 1718-1724. Cui Z J, Li Z X, Chen Z L, Zhao C P, Zheng S H, Zhou L Q. 2012. A study on the new method for determining small earthquake sequence type: Correlation analysis of spectral amplitude[J]. Chinese Journal of Geophysics, 55(5): 1718-1724 (in Chinese).
付虹, 黄浩, 李丽, 赵小艳. 2011. 2011年3月10日云南盈江5.8级地震序列研究[J]. 地震研究, 34(4): 414-419. Fu H, Huang H, Li L, Zhao X Y. 2011. Research of the March 10, 2011, MS5.8, Yingjiang, Yunnan earthquake sequence[J]. Journal of Seismological Research, 34(4): 414-419 (in Chinese).
黄玉龙, 郑斯华, 刘杰, 赵兴权, 康英. 2003. 广东地区地震动衰减和场地响应的研究[J]. 地球物理学报, 46(1): 54-61. Huang Y L, Zheng S H, Liu J, Zhao X Q, Kang Y. 2003. Attenuation of ground motion and site response in Guangdong region[J]. Chinese Journal of Geophysics, 46(1): 54-61 (in Chinese).
蒋海昆, 傅征祥, 刘杰. 2007. 中国大陆地震序列研究[M]. 北京: 地震出版社: 38-51. Jiang H K, Fu Z X, Liu J. 2007. Research of Earthquake Sequences in China[M]. Beijing: Seismological Press: 38-51 (in Chinese).
王俊国, 刁桂苓. 2005. 千岛岛弧大震前哈佛大学矩心矩张量(CMT)解一致性的预测意义[J]. 地震学报, 27(2): 178-183. Wang J G, Diao G L. 2005. Consistent CMT solutions from Harvard University before the great earthquakes in Kurile Islands and its significance for earthquake prediction[J]. Acta Seismologica Sinica, 27(2): 178-183 (in Chinese).
王兰兰, 刘丽芳. 2004. 云南地区4级地震频度异常特征与强震关系研究[J]. 内陆地震, 18(4): 359-364. Wang L L, Liu L F. 2004. Study on the relation between frequency anomalous characteristics of M4.0 earthquakes and strong earthquakes[J]. Inland Earthquake, 18(4): 359-364 (in Chinese).
吴开统, 焦远碧, 吕培苓, 王志东. 1990. 地震序列概论[M]. 北京: 北京大学出版社: 97-114. Wu K T, Jiao Y B, Lü P L, Wang Z D. 1990. Conspectus of Earthquake Sequences[M]. Beijing: Peking University Press: 97-114 (in Chinese).
赵英萍, 刁桂苓, 高景春, 王勤彩, 杜迎春, 朱振兴. 2004. 张北强余震前震源机制解的一致性特征[J]. 华北地震科学, 22(1): 1-4. Zhao Y P, Diao G L, Gao J C, Wang Q C, Du Y C, Zhu Z X. 2004. Consistency of the focal mechanisms before some strong aftershocks in Zhangbei earthquake series[J]. North China Earthquake Sciences, 22(1): 1-4 (in Chinese).
Atkinson G M, Mereu R F.1992. The shape of ground motion attenuation curves in southeastern Canada[J]. Bull Seismol Soc Am, 82(5): 2014-2031.
Brune J N.1970. Tectonic stress and the spectra of seismic shear waves from earthquake[J]. J Geophy Res, 75(26): 4997-5009.
Chael E. 1987. Spectral scaling of earthquakes in the Miramichi region of New Brunswick[J]. Bull Seismol Soc Am, 77(2): 347-365.
Lund B, Böðvarsson R. 2002. Correlation of microearthquake body-wave spectral amplitudes[J]. Bull Seismol Soc Am, 92(6): 2419-2433.
Moya A, Jorge A. 2000. Inversion of source parameters and site effects from strong ground motion records using genetic algorithms[J]. Bull Seismol Soc Am, 90(4): 977-992.
Wiemer S,Wyss M. 2002. Mapping spatial variability of the frequency-magnitude distribution of earthquakes[J]. Advances in Geophysics, 45: 259-302.
-
期刊类型引用(15)
1. 赵小艳,蒋海昆,孟令媛,苏有锦,贺素歌. 基于决策树的川滇地区地震序列类型判定特征重要性研究. 地震研究. 2024(03): 321-335 . 百度学术
2. 蒋海昆,王锦红. 适用于机器学习的地震序列类型判定特征重要性讨论. 地震研究. 2023(02): 155-172 . 百度学术
3. 马倩雯,宋春燕,陈勇,郭寅,张琳琳. 库车东南震群谱振幅相关系数特征分析. 内陆地震. 2023(04): 373-380 . 百度学术
4. 付虹,刘自凤,胡小静,李智蓉,洪敏,彭关灵,王光明,倪喆. 2021年云南漾濞M_S6.4地震异常跟踪分析. 地震研究. 2021(03): 301-308 . 百度学术
5. 赵小艳,王光明,张潜,贺素歌,樊文杰,刘自凤. 2021年云南漾濞M_S6.4地震序列特征及强余震判定. 地震研究. 2021(03): 309-319 . 百度学术
6. 杨士超,张博,曹凤娟,王亮,邵媛媛. 盖州震群谱振幅相关系数的研究. 地震. 2019(03): 158-165 . 百度学术
7. 李宏伟,王霞,宋美琴,吴昊昱. 2016年运城盐湖序列谱振幅相关系数变化特征. 地震地磁观测与研究. 2017(03): 35-40 . 百度学术
8. 周少辉,蒋海昆. 前震研究进展综述. 地震. 2016(03): 1-13 . 百度学术
9. 袁丽文,李强,陈智勇. 福建水口及仙游地震序列的谱振幅相关系数变化特征. 华南地震. 2016(03): 35-42 . 百度学术
10. Zhou Shaohui,Jiang Haikun. A Review on Research of Foreshocks. Earthquake Research in China. 2016(04): 470-484 . 必应学术
11. 倪红玉,刘泽民,洪德全,汪小厉,赵朋. 综合研究2014年霍山M_S4.3地震序列的震源机制变化过程. 地震地质. 2015(04): 1004-1019 . 百度学术
12. 黄显良,刘泽民,郁建芳,倪红玉,张炳,王琐琛. 2014年安徽金寨M_L3.9震群序列震源一致性研究. 地震学报. 2015(06): 916-924+1 . 本站查看
13. 崔子健,李志雄,陈章立. 云南景谷M_S6.6、云南沧源M_S5.5地震谱振幅相关系数特征分析. 地震研究. 2015(04): 535-540+697 . 百度学术
14. 崔子健,李志雄,陈章立,邵志刚. 中国东北2次中强地震谱振幅相关系数研究. 中国地震. 2015(02): 218-226 . 百度学术
15. 黄浩,付虹,王培玲,马玉虎. 云南鲁甸6.5级地震序列的谱振幅相关系数变化特征. 地震研究. 2014(04): 532-536 . 百度学术
其他类型引用(0)