首页> 外文期刊>Annals Of Geophysics >High precision leveling survey following the Md 4.0 Casamicciola earthquake of August 21, 2017 (Ischia, Southern Italy): field data and preliminary interpretation
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High precision leveling survey following the Md 4.0 Casamicciola earthquake of August 21, 2017 (Ischia, Southern Italy): field data and preliminary interpretation

机译:2017年8月21日(意大利南部伊斯基亚)Md 4.0卡萨米乔拉地震后的高精度水准测量:现场数据和初步解释

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The aim of this paper is the presentation of the results obtained from the high precision leveling survey carried out from November 6 to 11, 2017, in the area hit by the M d 4.0 Casamicciola earthquake of August 21, 2017, and critical discussion of these results in the light of the possible seismic source models. The measurements have been carried out on benchmarks of the northwestern sector of the altimetric network of the Ischia island, in the epicentral area. The heights of each benchmark have been obtained considering the historical reference benchmark n.1 located at Ischia Porto, and have been compensated over the whole stretch of the measured network; such heights have also been compared with those derived from the previous leveling campaign that was performed along the entire network in June 2010. The results obtained from the specific investigated leveling lines, which are considered representative of the kinematics of the northwestern area of the island, show conspicuous anomalies of ground deformation in the epicentral area of the August 21, 2017 earthquake. In particular, a significant ground subsidence of about 3.5 centimeters has been found between the benchmarks n. 92 and n. 98A along the “Borbonica Line”, quite anomalous compared to the previous measurements. Such subsidence located between the Piazza Maio (Casamicciola) and Fango (Lacco Ameno) localities, results spatially correlated with the deformation detected by the InSAR data analysis and coincides with the greatest macroseismic damages and with the coseismic surface fracture systems E-W oriented. Future leveling campaign in the area would be very crucial in order to follow and define the rate of postseismic motion of the seismogenetic source, also contributing with independent and valuable data to the seismic hazard knowledge of the Ischia island.
机译:本文的目的是介绍2017年11月6日至11日在2017年8月21日的Md 4.0卡萨米乔拉地震袭击的地区进行的高精度水准测量的结果,并对这些问题进行批判性讨论根据可能的地震源模型得出结果。这些测量是在震中地区伊斯基亚岛的高空网络西北段的基准上进行的。考虑到位于伊斯基亚波尔图的历史参考基准n.1,获得了每个基准的高度,并在整个测量网络范围内对其进行了补偿;此类高度也已与2010年6月沿整个网络进行的上次水准测量活动得出的高度进行了比较。从特定的调查水准测量线获得的结果被认为是该岛西北地区的运动学的代表,显示2017年8月21日地震震中区域的地面变形明显异常。特别是,在基准n之间发现了大约3.5厘米的明显地面沉降。 92和n。沿“ Borbonica Line”的98A,与以前的测量相比异常。这种沉陷位于马约广场(Casamicciola)和方戈(Lacco Ameno)地区之间,其结果与InSAR数据分析检测到的变形在空间上相关,并且与最大的宏观地震破坏以及E-W定向的同震表面裂缝系统相吻合。为了跟踪和定义地震发生源的地震后运动速度,该地区未来的水平运动将非常重要,这也将为伊斯基亚岛的地震灾害知识提供独立而有价值的数据。

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