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[1]田优平,沈 平,万永革,等.湖南地区应力场定量结果及置信区间分析[J].地震研究,2023,46(04):483-490.[doi:10.20015/j.cnki.ISSN1000-0666.2023.0052 ]
 TIAN Youping,SHEN Ping,WAN Yongge,et al.Quantitative Results and Confidence Interval Analysis of the Stress Field in Hunan Region[J].Journal of Seismological Research,2023,46(04):483-490.[doi:10.20015/j.cnki.ISSN1000-0666.2023.0052 ]
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湖南地区应力场定量结果及置信区间分析(PDF/HTML)

《地震研究》[ISSN:1000-0666/CN:53-1062/P]

卷:
46
期数:
2023年04期
页码:
483-490
栏目:
出版日期:
2023-07-15

文章信息/Info

Title:
Quantitative Results and Confidence Interval Analysis of the Stress Field in Hunan Region
作者:
田优平1沈 平1万永革23唐红亮1康承旭1姚海东1佘旭明1叶世山4
(1.湖南省地震局 湖南省震灾风险防治中心,湖南 长沙 410004; 2.防灾科技学院,河北 三河 065201; 3.河北省地震动力学重点实验室,河北 三河 065201; 4.广东省地震局,广东 广州 510070)
Author(s):
TIAN Youping1SHEN Ping1WAN Yongge23TANG Hongliang1KANG Chengxu1YAO Haidong1SHE Xuming1YE Shishan4
(1.Hunan Earthquake Disaster Risk Prevention Center,Hunan Earthquake Agency,Changsha 410004,Hunan,China)(2.Institute of Disaster Prevention,Sanhe 065201,Hebei,China)(3.Hebei Key Laboratory of Earthquake Dynamics,Sanhe 065201,Hebei,China)(4.Guangdong Earthquake Agency,Guangzhou 510070,Guangdong,China)
关键词:
应力场 格点尝试法 网格搜索法 置信区间 湖南地区
Keywords:
stress field the grid-trial method the grid-search method confidence interval Hunan region
分类号:
P315.727
DOI:
10.20015/j.cnki.ISSN1000-0666.2023.0052
摘要:
基于湖南及其邻区312个地震的529条P波初动极性数据和32个ML≥2.8地震的震源机制解,采用格点尝试法和网格搜索法分别反演得到了湖南地区构造应力场的定量结果和置信范围。格点尝试法计算得到的P轴方位和倾伏角分别为102°和10°,T轴方位和倾伏角分别为237°和76°; 网格搜索法反演得到的P轴方位和倾伏角分别为100°(置信区间为79°~100°)和5°(置信区间为2°~5°),T轴方位和倾伏角分别为225°(置信区间为204°~225°)和81°(置信区间为81°~82°)。结果表明:湖南地区平均震源机制解表现为逆断型; 主压应力轴优势方位为NWW向,倾伏角近乎水平; 主张应力轴优势方位为NE—NEE向,倾伏角较大。对两种方法得到的研究区应力场结果进行了可靠性分析并与前人结果进行了对比,证实本文结果的可信度较高。
Abstract:
Based on 529 P-wave polarity data of 312 earthquakes and the focal mechanism of 32 earthquakes with magnitude over 2.8 in Hunan and its neighboring region,we obtain the quantitative results and confidence ranges of the tectonic stress field in Hunan region by using the grid trial method and the grid search method respectively.The mean stress field calculated by the grid trial method shows that the azimuth of P-axis is 102°,the dip angle of P-axis is 10°,and the azimuth and dip angle of T-axis are 237° and 76° respectively.The results from the grid search inversion show that the azimuth and dip angle of P-axis are 100° when confidence interval is 79°-100°,and 5° when confidence interval is 2°-5°,and the azimuth and dip angle of T-axis are 225° when confidence interval is 204°-225°,and 81° when confidence interval is 81°-82°.According to the results of two stress field algorithms,the average focal mechanism proves to be reverse fault in Hunan region.The dominant direction of the principal compressive stress is NWW,and its dip angle is almost horizontal.The dominant direction of the principal tensile stress is NE-NEE,and its dip angle is large.We analyze the reliability of the inversion results from two algorithms,and compare with the previous study,and prove that the results proposed in this paper is of high reliability.

参考文献/References:

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备注/Memo

备注/Memo:
收稿日期:2022-05-09.
基金项目:中国地震局2022年度震情跟踪定向工作任务资助课题(2022010121); 湖南省地震局防震减灾科研课题(202303); 国家自然科学基金项目(41674055,42174074).
第一作者简介:田优平(1988-),工程师,主要从事计算地震学、地球动力学等研究.E-mail:tianyouping1123@163.com.
通讯作者简介:唐红亮(1979-),正高级工程师,主要从事地震大数据分析、地震业务信息化研究.E-mail:thl2222@126.com.
更新日期/Last Update: 2023-10-01