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Analysis of the strong motion data associated with normal fault mechanism earthquakes in Turkey

机译:与土耳其正常断层机制地震有关的强运动数据分析

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Strong motion data associated with the main-shock and after-shocks of the 1995 Dinarand 1997 Antakya, Turkey earthquakes have been analyzed to investigate the source, attenuationand site response parameters. Both earthquakes resulted from predominantly normal faulting.Dinar earthquake (Mw=6.0, USGS) occurred on October 1, 1995 causing casualties and physicaldamage (Io=VII-VIII MSK). The PGA in Dinar was 0.33g. The main-shock of the Antakya earthquaketook place on January 22, 1997 (Mw=5.8). Limited physical damage (Io=VI-VII MSK) wasconcentrated in the Hatay province. The PGA in Antakya was 0.15g. For both earthquakes, strongmotion data were baseline corrected, local magnitudes were computed and anelastic attenuation parameters,seismic moments and corner frequencies were assessed. It is believed that the obtaineddata will complement the relatively scarce earthquake data associated with extensional regimes.
机译:与1995年第纳尔主震和余震相关的强运动数据 对1997年土耳其安塔基亚地震进行了分析,以调查震源,衰减 和网站响应参数。两次地震都是主要由正常断层引起的。 第纳尔地震(Mw = 6.0,USGS)发生在1995年10月1日,造成人员伤亡和人身伤害。 损坏(Io = VII-VIII MSK)。第纳尔的PGA为0.33克。安塔基亚地震的主震 于1997年1月22日举行(Mw = 5.8)。有限的物理伤害(Io = VI-VII MSK)为 集中在哈塔伊省。安塔基亚(Antakya)的PGA为0.15克。对于两次地震, 对运动数据进行了基线校正,计算了局部震级并计算了非弹性衰减参数, 评估了地震力矩和转折频率。据认为,获得 数据将补充与扩展方案相关的相对稀少的地震数据。

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