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Synthesis of magnitude and focal mechanism computations for the M ≥ 4.5 earthquakes in France for the period 1995-2000

机译:1995年至2000年法国M≥4.5级地震的震级和震源机制计算的综合

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摘要

This paper proposes a synthesis of the studies made in terms of source parameters evaluation for the last earthquakes of local magnitude greater than 4.5 which occurred in or nearby France during the last five years. Focal mechanisms and seismic moments have been computed for the three most important events, largely felt by the population: St Paul de Fenouillet (February 18~(th) 1996, M_L 5.6), Annecy-Epagny (July 15~(th) 1996, M_L 5.2) and St-Beat (October 4~(th) 1999, M_L 4.8). These focal mechanisms have been obtained either by regional moment tensor inversion or from first motion polarities and are compared with complementary studies made on these earthquakes. In addition, for the other earthquakes of local magnitude greater than 4.5 which occurred nearby French borders since the beginning of the recording of broadband data by the ReNaSS (Reseau National de Surveillance Sismique, French Seismological Survey) in mid-1995, several magnitude calculations concerning the following earthquakes are presented: Pamplona (25/2/1996, M_L 4.7) Aoste (31/03/1996, M_L 4.6), Imperia (24/2/1997, M_L 4.5), Barcelonette (31/10/1997, M_L 4.8), Pamplona (27/10/1998, M_L 4.9), and Bonifacio (26/4/2000, M_L 4.5). Local magnitudes are usually higher than the M_b magnitudes reported by the PDE (Preliminary Determination of Epicenters), while the extension of the Msz scale to regional magnitudes and the Mw magnitudes derived from seismic moments give smaller values. The relative importance of the various earthquakes in terms of surface wave magnitude or seismic moment does not always agree with that implied by local magnitudes.
机译:本文提出了在过去五年中在法国或其附近发生的最后一次大于4.5级的最近地震的震源参数评估方面所做研究的综合报告。已计算出三个最重要的事件的震源机制和地震矩,这些事件在很大程度上引起了人们的注意:St Paul de Fenouillet(1996年2月18日至1990年5月5.6日),Annecy-Epagny(Anncyy-Epagny)(1996年7月15日至7月15日), M_L 5.2)和St-Beat(1999年10月4日),M_L 4.8)。这些震源机制是通过区域矩张量反演或首次运动极性获得的,并与对这些地震的补充研究进行了比较。此外,自ReNaSS(法国地震调查局国家地震监测所)于1995年中期开始记录宽带数据以来,在法国边界附近发生的其他当地地震级别大于4.5的其他地震中,涉及到的几个震级计算呈现以下地震:潘普洛纳(25/2/1996,M_L 4.7)奥斯特(31/03/1996,M_L 4.6),因佩里亚(24/2/1997,M_L 4.5),巴塞罗那(31/10/1997,M_L 4.8),潘普洛纳(1998年10月27日,M_L 4.9)和博尼法乔(Bonifacio)(26/4/2000,M_L 4.5)。局部震级通常高于PDE(震中的初步确定)报告的M_b震级,而Msz尺度的扩展到区域震级和地震矩得出的Mw震级给出较小的值。就地表波震级或地震矩而言,各种地震的相对重要性并不总是与局部震级所暗示的相对一致。

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