利用宽频带数字地震资料测定地震震级的方法研究
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摘要
在国际地震学与地球内部物理学联合会(IASPEI)新推荐震级标度在中国地震台网中心应用的基础上,提出中国地震台网地震震级测定方法。研究指出,地方性震级M_L与不同地区的地震波衰减特性具有密切关系,区域性特征明显,为保证中围地方性震级的一致性,宜沿用中国传统测定方法。建议:用IASPEI新推荐的短周期体波震级m_b和宽频带体波震级m_B(BB),分别取代中国传统的短周期体波震级m_b和中长周期体波震级m_B;用IASPEI新推荐的20 s面波震级M_S(20)、宽频带面波震级M_S(BB),分别取代中国传统面波震级M_S7与M_S。为使震级测定规范统一,给出新的震级计算公式和测定方法,并给出新旧震级之间的转换公式。采用新震级标度,可以充分发挥宽频带数字地震资料优势,使中国震级测定与国际接轨。
Based on the application of the new recommended magnitude scale by International Association of Seismology and Physics of the Earth s Interior(IASPEI)in China Earthquake Networks Center(CENC),we have proposed the method of magnitude measurement of China seismic network in this paper. The study indicated that local magnitude M_L has close relation with attenuation of seismic waves in different areas,which has obvious regional characteristic.In order to continue the coherent of our local magnitude,the traditional method is reserved.In order to bring all superiority of broadband digital seismic data into full play and be able to connect with international magnitude measurement,we recommend using new IASPEI short period body wave magnitude mb and broadband body wave magnitude m_B(BB)to replace traditional short period body wave magnitude m_b and medium and long period body wave magnitude m_B and using IASPEI new surface wave magnitude around 20 s M_S(20),broadband surface magnitude M_S(BB)replace our traditional surface wave magnitude M_(S7)and M_S.To make magnitude measurement standard unification,this paper gives the computing formulation and measurement method of new magnitude.When the new magnitude scale replaced the traditional ones,there will be difference between the new measurement and the old,the conversion equation was given in this paper.
Based on the application of the new recommended magnitude scale by International Association of Seismology and Physics of the Earth s Interior(IASPEI)in China Earthquake Networks Center(CENC),we have proposed the method of magnitude measurement of China seismic network in this paper. The study indicated that local magnitude M_L has close relation with attenuation of seismic waves in different areas,which has obvious regional characteristic.In order to continue the coherent of our local magnitude,the traditional method is reserved.In order to bring all superiority of broadband digital seismic data into full play and be able to connect with international magnitude measurement,we recommend using new IASPEI short period body wave magnitude mb and broadband body wave magnitude m_B(BB)to replace traditional short period body wave magnitude m_b and medium and long period body wave magnitude m_B and using IASPEI new surface wave magnitude around 20 s M_S(20),broadband surface magnitude M_S(BB)replace our traditional surface wave magnitude M_(S7)and M_S.To make magnitude measurement standard unification,this paper gives the computing formulation and measurement method of new magnitude.When the new magnitude scale replaced the traditional ones,there will be difference between the new measurement and the old,the conversion equation was given in this paper.
引文
陈培善.地震震级的综合评述[J].地震地磁观测与研究,1982,3(3) :14-19．
陈运泰,刘瑞丰.地震的震级[J].地震地磁观测与研究,2004,25(6) :1-11．
许绍燮,陆远忠,郭履灿,陈培善,许忠淮,肖承邺,冯义钧.地震震级的规定(GB17740-1999) [S].北京:中国标准出版社,1994 :1-5．
中国地震局.地震及前兆数字观测技术规范(地震观测)[S].北京:地震出版社,2001．
中国地震局.地震参数--数字地震学在地震预报中的应用[M].北京:地震出版社,2003．
Bormann P,Liu R F,Xu Z G,Ren K X,Zhang L W,Wendt S.First Application of the New IASPEI teleseismic magnitude standards to data of the China National Seismographic Network[J].Bull Seism Soc Amer,2009,99(3) :1 868-1 891．
Gutenberg B.Amplitude of surface waves and magnitude of shallow earthquakes[J].Bull Seism Soc Amer,1945a,35:3-12．
Gutenberg B.Amplitudes of P,PP,and S and magnitude of shallow earthquakes[J].Bull Seism Soc Amer,1945b,35:57-69．
Gutenberg B.and Richter C F.Magnitude and energy of earthquakes[J].Annali di Geofisica,1956,91:1-15．
IASPEI.Summary of Magnitude Working Group recommendations on standard procedures for determining earthquake magnitudes from digital data[EP/AL].http://www.iaspei.org/commissions/CSOI.html,2005．
Richter C F.An instrumental earthquake magnitude scale[J].Bull Seism Soc Amer,1935,25:1-32．
陈运泰,刘瑞丰.地震的震级[J].地震地磁观测与研究,2004,25(6) :1-11．
许绍燮,陆远忠,郭履灿,陈培善,许忠淮,肖承邺,冯义钧.地震震级的规定(GB17740-1999) [S].北京:中国标准出版社,1994 :1-5．
中国地震局.地震及前兆数字观测技术规范(地震观测)[S].北京:地震出版社,2001．
中国地震局.地震参数--数字地震学在地震预报中的应用[M].北京:地震出版社,2003．
Bormann P,Liu R F,Xu Z G,Ren K X,Zhang L W,Wendt S.First Application of the New IASPEI teleseismic magnitude standards to data of the China National Seismographic Network[J].Bull Seism Soc Amer,2009,99(3) :1 868-1 891．
Gutenberg B.Amplitude of surface waves and magnitude of shallow earthquakes[J].Bull Seism Soc Amer,1945a,35:3-12．
Gutenberg B.Amplitudes of P,PP,and S and magnitude of shallow earthquakes[J].Bull Seism Soc Amer,1945b,35:57-69．
Gutenberg B.and Richter C F.Magnitude and energy of earthquakes[J].Annali di Geofisica,1956,91:1-15．
IASPEI.Summary of Magnitude Working Group recommendations on standard procedures for determining earthquake magnitudes from digital data[EP/AL].http://www.iaspei.org/commissions/CSOI.html,2005．
Richter C F.An instrumental earthquake magnitude scale[J].Bull Seism Soc Amer,1935,25:1-32．
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