[1]陈珊桦,全建军,蔡佩蕊,等.泉州地震台M2166超宽频带地震仪记录的地球球型自由振荡信息研究[J].华南地震,2019,39(增刊):102-108.[doi:10.13512/j.hndz.2019.S1.017]
 CHEN Shanhua,QUAN Jianjun,CAI Peirui,et al.Study on Spherical Earth Free Oscillation Recorded by M2166 very Broadband Seismograph in Quanzhou Seismic Station[J].South China journal of seismology,2019,39(增刊):102-108.[doi:10.13512/j.hndz.2019.S1.017]
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泉州地震台M2166超宽频带地震仪记录的地球球型自由振荡信息研究()
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华南地震[ISSN:1006-6977/CN:61-1281/TN]

卷:
39
期数:
2019年增刊
页码:
102-108
栏目:
华南地震
出版日期:
2019-10-31

文章信息/Info

Title:
Study on Spherical Earth Free Oscillation Recorded by M2166 very Broadband Seismograph in Quanzhou Seismic Station
作者:
陈珊桦1全建军2蔡佩蕊3林加宝4张有明1罗开奇1
1. 福建省地震局泉州基准地震台,福建 泉州 362000;2. 福建省地震局永安地震台,福建 永安 366000; 3. 福建省地震局莆田地震台,福建 莆田 351100;4. 福建省地震局,福州 350003
Author(s):
CHEN Shanhua1QUAN Jianjun2CAI Peirui3LIN Jiabao4ZHANG Youming1LUO Kaiqi1
1.Quanzhou Basic Seismic Station,Fujian Earthquake Agency,Quanzhou 362000,China;2. Yongan Seismic Station, Fujian Earthquake Agency,Yongan 366000,China;3. Putian Seismic Station,Fujian Earthquake Agency,Putian 351100,China;4. Fujian Earthquake Agency,Fuzhou 350003,China
关键词:
M2166地震仪地球自由振荡球型振荡功率谱密度
Keywords:
M2166 seismographEarth Free oscillationSpherical oscillationPower spectral density
DOI:
10.13512/j.hndz.2019.S1.017
文献标志码:
A
摘要:
利用泉州基准地震台M2166超宽频带地震仪记录的7个MS≥8.0地震震后5天数据资料,采用功率谱密度估计方法,提取到73个基频振型(0S4~0S76)和多个谐频振型,各振型频率点与地球初步参考模型(PREM)理论频率值符合较好,利用3套超宽频带地震仪数据对球型自由振荡信息能量分布差异进行探究,认为地球介质的横向不均匀性和各向异性是造成差异的主要原因。得到的结果可用于地球内部结构的研究,有助于做出更精细的地球模型。
Abstract:
By using the five days post-earthquake waveform data of seven earthquakes with MS≥8.0 which recorded by M2166 very broadband seismograph in Quanzhou seismic station. The 73 fundamental frequency modes(0S4~0S76)and many harmonic vibration modes were extracted by the power spectral density estimation method, it is found that the detected oscillation frequencies are in good agreement with the theoretical frequency of the PREM model. The difference of the energy distribution of free-oscillation information was studied by using three very broadband seismograph data, it is considered that the lateral heterogeneous or anisotropic media of the earth is the main cause of the difference. These free oscillation information can be used in the study of the earth’s internal structure and help to make a more detailed earth model.

备注/Memo

备注/Memo:
收稿日期:2019-02-26 基金项目:国家自然科学基金面上项目(41676025);2017年福建省地震局科技基金专项(SF201701) 作者简介:陈珊桦(1989- ),女,工程师,主要从事地震监测与数字地震应用工作。 E-mail:susanna_csh@163.com.
更新日期/Last Update: 2019-12-06