基于五大连池火山区域地方震资料,选取信噪比高、定位准确且震中位于火山区域的39个地震,根据地震波传播的三段几何衰减模型,使用地震记录位移谱,去除仪器响应、背景噪声,反演求取各频点f的S波Q值,拟合获得火山区体波Q值与f的关系为Q(f)=221.7f0.452,计算得到老黑山、火烧山附近区域Q值与f的关系为Q(f)=152f0.600,与国内外其他区域体波Q值进行对比,并结合火山区地质构造活动,分析五大连池火山区体波Q值特征。
using the local earthquake data of wudalianchi area, which are from selected 39 earthquakes with accurate locations and high noise-signal ratio, according to the three part decaying model in the course of seismic wave transmission, we reverse data and calculate Q value of S wave and obtain the result Q(f)=221.7f0.452 in Wudalianchi volcano area with the seismic displacement spectrum after eliminating instrument response and background noise. At the same time we also get the result Q(f)=152f0.600 in the zone below Laohei and Huoshao mount. In the end we get some conclusion from the results by comparing with other Q value of other area.
2018,39(5): 23-29 收稿日期:2018-04-23
DOI:10.3969/j.issn.1003-3246.2018.05.004
作者简介:高亮(1982-),男,湖北监利人,研究生,工程师,现从事地震监测与分析工作。E-mail:176037242@qq.com
参考文献:
高亮,张守国,闫峰. 五大连池火山区尾波Q值研究[J]. 地震地磁观测与研究,2013,34(1/2):41-46.
梁国经,李仲巍,郑双凤,等. 龙岗火山区尾波Q值的初步研究[J]. 地震地质,2011,33(1):114-122.
彭年,刘永顺,韦玉凤. 五大连池新期火山岩浆房动力稳定性探讨[J]. 岩石矿物学杂志,2005,24(3):198-204.
张凤鸣,张守国,邹卫东. 五大连池火山构造地震空间分布及其构造含义[J]. 东北地震研究,1996,12(4):17-22.
赵谊,邹卫东,周皓. 五大连池火山危险性分析[J]. 自然灾害学报,1999,8(4):140-146.
Aki K. Attenuation of shear-waves in the lithosphere for frequencies from 0.05 to 25 Hz[J]. Physics of the Earth and Planetary Interiors, 1980, 21(1):56-60.
Aki K. Scattering and attenuation of shear waves in the lithosphere[J]. Journal of Geophysical Research:Solid Earth, 1980, 85(B11):6 496-6 504.
Atkinson G M, Mereu R F. The shape of ground motion attenuation curves in southeastern Canada[J]. Bull Seismol Soc Am, 1992, 82(5):2 014-2 031.