The L'Aquila seismic swarm culminated with the mainshock of April 6, 2009 (ML ¼ 5.9). Here, we report and analyze the Large Volume Detector (LVD, used in neutrinos research) low energy traces (~0.8 MeV), collected during the early-mid stages of the seismic sequence, together with the data of a radon monitoring experiment. The L'Aquila seismic swarm culminated with the mainshock of April 6, 2009 (ML 5.9). Here, we report and analyze the Large Volume Detector (LVD, used in neutrinos research) low energy traces (~0.8 MeV), collected during the early-mid stages of the seismic sequence, together with the data of a radon monitoring experiment.
The LVD signals during the early-mid stages of the L'Aquila seismic sequence and the radon signature of some aftershocks of moderate magnitude
CIGOLINI, Corrado;LAIOLO, Marco;COPPOLA, DIEGO
2015-01-01
Abstract
The L'Aquila seismic swarm culminated with the mainshock of April 6, 2009 (ML ¼ 5.9). Here, we report and analyze the Large Volume Detector (LVD, used in neutrinos research) low energy traces (~0.8 MeV), collected during the early-mid stages of the seismic sequence, together with the data of a radon monitoring experiment. The L'Aquila seismic swarm culminated with the mainshock of April 6, 2009 (ML 5.9). Here, we report and analyze the Large Volume Detector (LVD, used in neutrinos research) low energy traces (~0.8 MeV), collected during the early-mid stages of the seismic sequence, together with the data of a radon monitoring experiment.
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Cigolini_JER 2014 man final.pdf
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