西西里岛东南部的震源和地震危险性

M. S. Barbano, R. Rigano
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引用次数: 39

摘要

对影响西西里岛东南部的一些地震(M > 5.3)进行了研究,以确定其震源并估计该地区的地震危险性。对历史报告的分析使我们能够使用新的欧洲宏观地震等级98重新评估1542年、1693年、1818年、1848年和1990年地震的强度。新的烈度数据用于确定参数和震源方向。将得到的震源与利用从意大利强震目录检索到的MCS强度计算得到的震源进行比较。所采用的程序给出的结果在统计上是显著的,但在某些情况下,震中位置和震源方位角都受到强度分布的方位角差距的强烈影响。这主要体现在1693年1月的地震中。对于这些地震,宏观地震数据的不确定性给出了明显不同的解,并且不允许将这些事件与已知的活动断层联系起来。通过处理新的烈度估计数据,利用现场地震历史资料,计算了部分地区的地震危险性。在卡塔尼亚、伦蒂尼和奥古斯塔之间的地区获得了破坏性事件发生的最高概率(I = 10),表明发震源位于爱奥尼亚海岸附近。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Earthquake sources and seismic hazard in Southeastern Sicily
A study of some earthquakes (M > 5.3) affecting Southeastern Sicily was performed to define their seismic sources and to estimate seismic hazard in the region. An analysis of historical reports allowed us to reassess intensities of the 1542, 1693, 1818, 1848 and 1990 earthquakes by using the new European Macroseismic Scale 98. The new intensity data were used to define parameters and the orientation of seismic sources. The sources obtained were compared with the ones computed using the MCS intensities retrieved from the Catalogue of Strong Italian Earthquakes. The adopted procedure gives results that are statistically significant, but both the epicentre location and source azimuth, in some cases, are strongly affected by the azimuthal gap in the intensity distribution. This is evident mainly for the 1693 January earthquakes. For these earthquakes the macroseismic data uncertainty gives significantly different solutions, and does not allow the events to be associated with known active faults. By handling the new estimated intensity data and using the site seismic histories, the seismic hazard for some localities was calculated. The highest probability of occurrence, for destructive events (I = 10), was obtained in the area between Catania, Lentini and Augusta, suggesting that the seismogenic sources are located near the Ionian coast.
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