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Seismicity at the border between the Southern and Central Apennines (Italy): a review

机译:南部和亚平宁山脉(意大利)之间边界的地震活动:回顾

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We review the instrumental seismicity at the boundary between the Southern and Central Apennines with the aim of detecting the active structures and clarifying the seismotectonic framework of this area of the chain. Single events with M<3.0, low magnitude (M<4.0) seismic sequences (1997-1998 and 2001), and swarms (1999, 2000 and 2005) characterize the seismicity of this area. Earthquakes occur within the upper 15 km of the crust, prevalently aligning along the Apennine Chain in a NW-SE axis. Strain analyses indicate that these events are related to the main NE-SW extension processes that affect the Apennine Chain. They are concentrated in the following areas: (a) south of the seismogenetic source responsible for the 1915 destructive earthquake (2000 swarm), (b) between the faults of the 1984 and 1805 destructive events (2001 sequence), and (c) between the faults of the 1805 and 1688 events (1997-1998 seismic sequence). The 1999, 2000 and 2005 swarms occurred along the so-called Ortona-Roccamonfina alignment, which is the NNE-SSW belt separating the Central Apennines from the Southern ones. The distribution of these swarms and the focal mechanisms indicate the presence of active NE-SW faults related to a local NW-SE extension. This direction of extension was also observed in the 1997-1998 and 2001 sequences. The location of the NE-SW striking faults, responsible for the seismic swarms, suggest that some segments of the Ortona-Roccamonfina line may be a rupture response to both the NE-SW regional extension of the Southern Apennines, and to a NW-SE striking longitudinal extension. Our data indicate that the seismicity of the Apennines at the boundary between the central and southern sectors is related to both the eastward migration of the chain (the NE-SW extension) and to its progressive curvature and thinning (the NW-SE extension). The NE-SW extension is responsible for the major earthquakes whereas the lower energy seismicity is related to the NW-SE extension.
机译:我们研究了南部和中部亚平宁山脉边界的仪器地震活动,目的是探测活动结构并弄清该链条区域的地震构造框架。 M <3.0,低震级(M <4.0)地震序列(1997-1998和2001)以及成群(1999、2000和2005)的单个事件是该地区地震活动的特征。地震发生在地壳的上15公里以内,通常沿着NW-SE轴的亚平宁链排列。应变分析表明,这些事件与影响亚平宁链的主要NE-SW延伸过程有关。它们集中在以下区域:(a)引起1915年破坏性地震(2000群)的地震成因源以南,(b)1984年和1805年破坏性事件的断层之间(2001序列),以及(c) 1805和1688事件的断层(1997-1998地震序列)。 1999年,2000年和2005年的蜂群沿着所谓的Ortona-Roccamonfina线发生,这是将中亚的亚平宁山脉与南部的亚西南亚分离的NNE-SSW带。这些群的分布和震源机制表明存在与本地NW-SE扩展有关的活动NE-SW故障。在1997-1998和2001序列中也观察到了这种扩展方向。负责地震群的NE-SW撞击断层的位置表明,Ortona-Roccamonfina线的某些部分可能是对南亚平宁山脉的NE-SW区域扩展和NW-SE的破裂响应。惊人的纵向延伸。我们的数据表明,亚平宁山脉在中部和南部扇形边界处的地震活动性与链条的东移(NE-SW扩展)及其渐进曲率和细化(NW-SE扩展)有关。 NE-SW扩展负责大地震,而较低能量的地震活动性与NW-SE扩展有关。

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