%0 Journal Article %1 weber_etal:2007 %A Weber, E. %A Convertito, V. %A Iannaccone, G. %A Zollo, A. %A Bobbio, A. %A Cantore, L. %A Corciulo, M. %A Di Crosta, M. %A Elia, L. %A Martino, C. %A Romeo, A. %A Satriano, C. %D 2007 %J Seismological Research Letters %K geophysics seismology %N 6 %P 622--634 %R 10.1785/gssrl.78.6.622 %T An advanced seismic network in the Southern Apennines (Italy) for seismicity investigations and experimentation with earthquake early warning %U http://dx.doi.org/10.1785/gssrl.78.6.622 %V 78 %X The last strong earthquake that occurred in the southern Apennines, the Irpinia earthquake on 23 November 1980 (M 6.9), was characterized by a complex rupture mechanism that ruptured three different faults (Bernard and Zollo 1989). This earthquake was well studied, and the quantity of data available has allowed a very detailed definition of the geometry and mechanisms of faults activated during this seismic event (Westaway and Jackson 1987; Pantosti and Valensise 1990).Even more than 20 years after the main event, the seismotectonic environment that contains the fault system on which the 1980 earthquake occurred shows continued background seismic activity including moderate-sized events such as the 1996 (M 5.1), 1991 (M 5.1) and 1990 (M 5.4) events. Moreover, the locations of the microearthquakes (taken from the database of the Istituto Nazionale di Geofisica e Vulcanologia, INGV) define an epicentral area with a geometry and extent surprisingly similar to that of the 1980 earthquake and its aftershocks. These simple observations suggest that it may be possible to study the preparation cycles of strong earthquakes on active faults by studying the microseismicity between seismic events. With this in mind, a seismic network of large dynamic range was planned and is now in an advanced phase of completion in the southern Apennines. Called ISNet (Irpinia Seismic Network), it is equipped with sensors that can record high-quality seismic signals from both small-magnitude and strong earthquakes, from which it will be possible to retrieve information about the rupture process and try to understand the scaling relationships between small and large events. 10.1785/gssrl.78.6.622

@article{weber_etal:2007, abstract = {The last strong earthquake that occurred in the southern Apennines, the Irpinia earthquake on 23 November 1980 (M 6.9), was characterized by a complex rupture mechanism that ruptured three different faults (Bernard and Zollo 1989). This earthquake was well studied, and the quantity of data available has allowed a very detailed definition of the geometry and mechanisms of faults activated during this seismic event (Westaway and Jackson 1987; Pantosti and Valensise 1990).Even more than 20 years after the main event, the seismotectonic environment that contains the fault system on which the 1980 earthquake occurred shows continued background seismic activity including moderate-sized events such as the 1996 (M 5.1), 1991 (M 5.1) and 1990 (M 5.4) events. Moreover, the locations of the microearthquakes (taken from the database of the Istituto Nazionale di Geofisica e Vulcanologia, INGV) define an epicentral area with a geometry and extent surprisingly similar to that of the 1980 earthquake and its aftershocks. These simple observations suggest that it may be possible to study the preparation cycles of strong earthquakes on active faults by studying the microseismicity between seismic events. With this in mind, a seismic network of large dynamic range was planned and is now in an advanced phase of completion in the southern Apennines. Called ISNet (Irpinia Seismic Network), it is equipped with sensors that can record high-quality seismic signals from both small-magnitude and strong earthquakes, from which it will be possible to retrieve information about the rupture process and try to understand the scaling relationships between small and large events. 10.1785/gssrl.78.6.622}, added-at = {2012-09-01T13:08:21.000+0200}, author = {Weber, E. and Convertito, V. and Iannaccone, G. and Zollo, A. and Bobbio, A. and Cantore, L. and Corciulo, M. and Di Crosta, M. and Elia, L. and Martino, C. and Romeo, A. and Satriano, C.}, biburl = {https://www.bibsonomy.org/bibtex/24911605c562cfbbdd9757cc746d5df38/nilsma}, day = 1, doi = {10.1785/gssrl.78.6.622}, interhash = {de86de521debd84c75bd95547bf08d28}, intrahash = {4911605c562cfbbdd9757cc746d5df38}, journal = {Seismological Research Letters}, keywords = {geophysics seismology}, month = nov, number = 6, pages = {622--634}, timestamp = {2021-02-09T13:24:56.000+0100}, title = {An advanced seismic network in the Southern Apennines (Italy) for seismicity investigations and experimentation with earthquake early warning}, url = {http://dx.doi.org/10.1785/gssrl.78.6.622}, volume = 78, year = 2007 }