基于Sato模型,采用2016年3月至2018年6月内蒙古东北部及临近地区发生的526次地震事件,挑选ML ≥ 2.0、记录清晰且信噪比较高的102次地震事件,拟合得到内蒙古东北部地区尾波Q值,得到QC(f)=(64.74 ±29.09)f(0.8925 ±0.0765);Q值与依赖指数η成反比,且该区北部Q值偏高,南部Q值偏低,可能与地质构造及地震活动性有关。
Based on the Sato model, 102 earthquake events with ML ≥ 2.0 and waveform clear records and high signal-to-noise ratio were selected from 526 earthquake events in the northeast of Inner Mongolia and adjacent areas from March 2016 to June 2018. The results of fitting Q value of coda wave in the northeast of Inner Mongolia is QC(f)=(64.74 ±29.09) f(0.8925 ±0.0765). The Q value is inversely proportional to the dependence index η, and the Q value in the north is higher and the Q value in the south is lower. May be related to tectonic and seismic activity.
2019,40(1): 48-52 收稿日期:2018-8-28
DOI:10.3969/j.issn.1003-3246.2019.01.005
基金项目:内蒙古自治区地震局局长基金(项目编号:2018JC05)
作者简介:翟浩(1990-),男,助理工程师,主要从事地震编目及系统运维工作。E-mail:496831965@qq.com
参考文献:
阿衣仙姑·买买提,尼鲁帕尔·买买吐孙. 基于Aki、Sato模型的阿克陶MS 6.7地震尾波Q值特征研究[J]. 内陆地震,2017,31(2):145-155.
李白基,秦嘉政,钱晓东,等. 云南姚安地区的尾波衰减[J]. 地震学报,2004,26(1):47-52.
刘芳,苗春兰,高艳玲. 内蒙古中西部地区尾波Q值研究[J]. 地震,2007,27(2):72-80.
马云生,张天中,张焕生. 北京及其周围地区尾波Q值分布特征的研究[J]. 地震学报,1995,17(1):448-458.
师海阔,曾宪伟,田小慧,等. 利用Sato模型研究宁夏及邻区尾波Q值分布特征[J]. 地震地磁观测与研究,2016,37(1):22-29.
王伟君,刘杰. 1999年岫岩地震序列尾波QC的变化过程[J]. 地震,2004,24(4):37-44.
朱新运,杨钢宇,张震峰. 基于Sato模型的近震S波尾波Q值求解及分析软件研制[J]. 地震地磁观测与研究,2005,26(3):63-70.
Aki K. Analysis of seismic coda of local earthquakes as scattered wave[J]. J Geophys Res, 1969, 74:615-631
Aki K. Cattering and attenuation of shear waves in the lithosphere[J]. J Geophys Res, 1980, 85:6 496-6 504.
Aki K, Chouet B. Origin of Coda wave:source, attenuation and scattering effects[J]. J Geophys Res, 1975, 80:3 322-3 342.
Chouet B. Temporal variation in the attenuation of earthquake coda near Stone Canyon, California[J]. Geophys Res Lett, 1979, 6(3):143-146.
Domingguez T and Rebollar C J. Attenuation of coda waves at the Cerro Prieto Geothermal Field, Baja California,Mexico[J]. Bull Seismol Soc Am, 1997, 87:1 368-1 374.
Jeffreys. On the transverse circulation in streams[J]. Mathematical Proceedings of the Cambridge Philosophical Society,1929,25(1).
Jin A S, Cao T Q, Aki K. Regional change of coda Q in the oceanic lithosphere[J]. J Geophys Res Solid Earth, 1985, 90(B10):8 651-8 659.
Pulli J J. Attenuation of coda waves in New England[J]. Bull Seismol Soc Am, 1984, 74(4):1 149-1 166.
Roecker S W, Tucker B, King J, et al. Estimates of Q in central Asia as a function of frequency and depth using the coda of locally recorded earthquakes[J]. Bull Seismol Soc Am, 1982, 72(1):129-149.
Sato H. Energy propagation including scattering effect:Single isotropic scattering,approximation[J]. Bull Seismol Soc Am, 1977, 68:923-948.
Singh S, Herrmann R B. Regionalization of crustal coda Q in the continental United Stated[J]. J Geophys Res Solid Earth, 1983, 88(B1):527-538.