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Local magnitude calibration of the Hellenic Unified Seismic Network

机译:希腊统一地震台网的局部震级校准

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摘要

A new relation is proposed for accurate determination of local magnitudes in Greece. This relation is based on a large number of synthetic Wood-Anderson (SWA) seismograms corresponding to 782 regional shallow earthquakes which occurred during the period 2007-2013 and recorded by 98 digital broad-band stations. These stations are installed and operated by the following: (a) the National Observatory of Athens (HL), (b) the Department of Geophysics of the Aristotle University of Thessaloniki (HT), (c) the Seismological Laboratory of the University of Athens (HA), and (d) the Seismological Laboratory of the Patras University (HP). The seismological networks of the above institutions constitute the recently (2004) established Hellenic Unified Seismic Network (HUSN). These records are used to calculate a refined geometrical spreading factor and an anelastic attenuation coefficient, representative for Greece and surrounding areas, proper for accurate calculation of local magnitudes in this region. Individual station corrections depending on the crustal structure variations in their vicinity and possible inconsistencies in instruments responses are also considered in order to further ameliorate magnitude estimation accuracy. Comparison of such calculated local magnitudes with corresponding original moment magnitudes, based on an independent dataset, revealed that these magnitude scales are equivalent for a wide range of values.
机译:提出了一种新的关系,用于准确确定希腊的局部震级。这种关系是基于大量的伍德·安德森(SWA)合成地震图,对应于2007年至2013年期间发生的782次区域浅震,并由98个数字宽带站记录。这些台站的安装和操作如下:(a)雅典国家天文台(HL),(b)塞萨洛尼基亚里士多德大学地球物理系(HT),(c)雅典大学地震实验室(HA)和(d)帕特雷大学(HP)的地震实验室。上述机构的地震网络构成了最近(2004年)建立的希腊统一地震网络(HUSN)。这些记录用于计算精确的几何扩展因子和无弹性衰减系数,代表希腊和周边地区,适合准确计算该地区的局部震级。为了进一步改善幅度估算的准确性,还考虑了根据其附近地壳结构变化以及仪器响应中可能存在的不一致进行的单个站校正。根据一个独立的数据集,将这些计算出的局部震级与相应的原始弯矩震级进行比较,结果表明,这些震级标度在很宽的范围内都是等效的。

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