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Dataset of seismic ambient vibrations from the quaternary Norcia basin (central Italy)

机译:第四纪诺西亚盆地(意大利中部)地震环境振动数据集

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摘要

Central Italy was affected by a long seismic sequence in 2016 and 2017, characterized by five main-shocks with Mw>5.0. The Mw 6.5 mainshock occurred on 30 October 2016 close to the town of Norcia, located in the intra-Apennine Norcia basin. Different degrees of damages were observed during this seismic crisis, caused by a variable seismic shaking. This was also due to important 1D and 2D variation of Quaternary fluvio-lacustrine sediments infilling the basin. Following such considerations, a new geophysical dataset of seismic vibration measurements was acquired in the study area during the period April 2017–November 2019. We collected mainly single-seismic station noise data, to infer the distribution of resonance frequency (f ) of the basin. A total of 60 sites were measured to cover the entire extension in the basin. We deployed seismometers along three transects of a total length of 21 km, mostly along the main structural directions of the basin (i.e. NNW-SSE and NE-SW). Two 2D arrays of seismic stations with a elicoidal-shaped geometry, and a set of MASW active data were also acquired in the northern sector of the basin, in order to better constrain the seismic velocity of the sedimentary infilling. These new records have been integrated with available geological information in order to reconstruct the deep structure of the basin, as discussed in the research paper by . The entire dataset used in is here provided, together with 7 additional records recovered for the basin (i.e. N54-N60) and ancillary open-source geospatial data. The dataset can be used for different purposes: specific research on the Norcia basin, comparative studies on similar areas around the world, development of new data modeling and testing of new analysis software, and as a training dataset for machine learning applications.
机译:意大利中部在2016年和2017年受到长地震序列的影响,其特征是5个主震Mw> 5.0。 6.5 Mw主震发生在2016年10月30日,靠近亚平宁内诺奇亚盆地的诺奇亚镇。在这次地震危机中,观察到了不同程度的破坏,这是由可变的地震震动引起的。这也是由于充满盆地的第四纪河流湖泊沉积物的重要一维和二维变化所致。基于这些考虑,在研究区域于2017年4月至2019年11月期间获得了一个新的地震振动地球物理数据集。我们主要收集了单地震台站噪声数据,以推断盆地的共振频率(f)的分布。 。总共测量了60个位置,以覆盖盆地的整个延伸。我们沿着三个总长度为21 km的样带部署了地震仪,主要沿盆地的主要结构方向(即NNW-SSE和NE-SW)进行了部署。为了更好地限制沉积物充填的地震速度,在盆地北部地区还采集了两个具有椭圆形几何形状的二维地震台站阵列和一组MASW活动数据。这些新记录已与可用的地质信息整合在一起,以重建盆地的深层结构,正如的研究论文所述。这里提供了中使用的整个数据集,以及为该盆地恢复的7条其他记录(即N54-N60)和辅助开源地理空间数据。该数据集可用于不同目的:对Norcia盆地的特定研究,对全球类似地区的比较研究,新数据模型的开发和新分析软件的测试,以及作为机器学习应用程序的训练数据集。

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