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2022-01-15汤加火山喷发的地震学震级测定 被引量:2

Surface Wave Magnitude Determination of Volcanic Eruption in Tonga on January 15,2022
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摘要 利用山东地震台网70个宽频带测震台站记录的2022-01-15南太平洋汤加海底火山喷发原始地震波形数据,从时间域和频率域分析火山喷发地震波的记录特征;通过对20 s优势周期面波进行研究,测算该次火山喷发的地震学震级与地震波辐射能量。研究表明,该次汤加火山喷发的面波震级为M_(S)5.674、能量震级为M_(e)5.704,与GFZ测定震级基本一致,比USGS测定震级小0.126。本次汤加火山爆炸指数(VEI)为5级,但本文测定的地震波辐射能量为8.155×10^(12)J,可见火山喷发以地震波辐射方式释放的能量较少,绝大部分能量以超过1000 km/h的冲击波形式穿过大气层迅速释放到空中,这种能量的快速释放会抑制深部应力的挤压与拉伸。 Using the original seismic waveform data of Tonga submarine volcanic eruption in the South Pacific on January 15,2022,recorded by 70 broadband stations of the Shandong seismic network,we analyze the recording characteristics of volcanic eruption seismic wave from time and frequency domains.By studying the surface wave with 20 s dominant period,we calculate the surface wave magnitude and seismic wave radiation energy of the volcanic eruption.The results show that the surface wave magnitude of the Tonga volcanic eruption is M_(S)5.674 and the energy magnitude is M_(e)5.704,which is basically consistent with the magnitude measured by GFZ and 0.126 smaller than that measured by USGS.The Tonga volcanic explosivity index(VEI)is grade 5,but the seismic wave radiation energy measured in this paper is 8.155×10^(12)J.The volcanic eruption releases less energy in the form of seismic wave radiation,and most of the energy is rapidly released into the air through the atmosphere in the form of shock wave with the speed more than 1000 km/h,inhibiting the compression and extension of deep stress.
作者 石玉燕 张春鹏 颜启 苗庆杰 SHI Yuyan;ZHANG Chunpeng;YAN Qi;MIAO Qingjie(Shandong Earthquake Agency,20 East-Wenhua Road,Ji’nan 250014,China)
机构地区 山东省地震局
出处 《大地测量与地球动力学》 CSCD 北大核心 2023年第2期209-214,共6页 Journal of Geodesy and Geodynamics
关键词 火山喷发 面波震级 台基校正 时频分析 地震波辐射能量 volcanic eruption surface wave magnitude site correction time frequency analysis seismic wave radiation energy
作者简介 第一作者:石玉燕,高级工程师,主要从事地震监测与数字地震学研究,E-mail:94759952@qq.com。
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  • 1陈运泰,刘瑞丰.地震的震级[J].地震地磁观测与研究,2004,25(6):1-12. 被引量:126
  • 2陈培善.面波震级测定的发展过程概述[J].地震地磁观测与研究,1989,10(6):1-9. 被引量:14
  • 3刘瑞丰,陈运泰,PETER BORMANN,任枭,侯建民,邹立晔,杨辉.中国地震台网与美国地震台网测定震级的对比(Ⅱ)——面波震级[J].地震学报,2006,28(1):1-7. 被引量:60
  • 4许绍燮.1994.地震震级的规定(GB17740-1999)[M].北京:中国标准出版社,1~5
  • 5郭履灿 庞明虎.面波震级和它的台基校正值[J].地震学报,1981,3(3):312-320.
  • 6国家地震局.地震台站观测规范[M].北京:地震出版社,1978.1-12.
  • 7陈培善 左兆荣 肖洪才.用763长周期地震仪台网测定面波震级.地震学报,1988,10(1):11-24.
  • 8Ambrasseys N N.1990.Uniform magnitude re-evaluation of European earthquakes associated with strong-motion records[J].Earthq Engin Structl Dyn,19:1-20.
  • 9Bormann P,Khalturin V I.1975.Relations between different kinds of magnitude determinations and their regional variations[C]// Proc ⅩⅣth General Assembly of the European Seismological Commission,Trieste,16-22 September 1974.Berlin:Nationalkomitee für Geod(a)sie und Geophysik,AdW der DDR:27-39.
  • 10Carroll R I,Ruppert D.1996.The use and misuse of orthogonal regression in linear errors-in-variables models[J].The American Statistician,50(1):1-6.

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