祁连山—六盘山地震带测震学参数分析
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摘要
测震学参数是目前常用的确定某区域内地震活动时、空、强特点、判断未来某区域地震活动趋势的主要方法。本文对祁连山—六盘山地震带中一些测震学参数b值、D值、A(b)值及GL值进行了分析研究,提出了该区域内中强震发生前以上四种测震学参数的变化特征,为今后利用测震学参数准确把握该带地震活动趋势提供了依据。
Occurrence of earthquakes in the region, in order to provide the basis for the trend of the seismic activities in the region by using seismological parameters in the fu Seismological parameters are currently the primary means to identify the spatial and intensity characteristics in seismic activities that determine the future trend of seismic activities in a region. In this paper, by means of studying part of the b value, D value, A(b) value and GL value in Qilian Mt.-Liupan Mt. Seismic Belts, we presented the variation of the four seismological parameters above before the ture.
Occurrence of earthquakes in the region, in order to provide the basis for the trend of the seismic activities in the region by using seismological parameters in the fu Seismological parameters are currently the primary means to identify the spatial and intensity characteristics in seismic activities that determine the future trend of seismic activities in a region. In this paper, by means of studying part of the b value, D value, A(b) value and GL value in Qilian Mt.-Liupan Mt. Seismic Belts, we presented the variation of the four seismological parameters above before the ture.
引文
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[2]国家地震局预测预防司[M].地震综合分析预方法,北京:地震出版社,1998.
[3]陈远忠,陈章立,等.地震预报的地震学方法[M].北京:地震出版社,1985.
[4]李金林,等.地震频度-震级关系的时空扫描[M].北京:地震出版社,1979.
[5]冯建刚等.甘肃测震台网监测能力及地震目录完整性分析[J].地震学报,2012,34,646-658.
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