2012
DOI: 10.1016/j.tecto.2012.01.008
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Retrospective investigation of geomagnetic field time-series during the 2009 L'Aquila seismic sequence

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Cited by 15 publications
(15 citation statements)
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“…Masci and Di Persio (2012) have shown that, while the horizontal components H and D have a strong similarity in the fractal time series, the Z component only sometimes (when it is more influenced by geomagnetic activity) shows the same fractal features of the other two components (see Fig. 4 by Masci and Di Persio, 2012). Bearing in mind these considerations, we should not expect a strong correlation between Kp and the fractal dimension of the Z component for a long time-series duration.…”
Section: Discussionmentioning
confidence: 91%
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“…Masci and Di Persio (2012) have shown that, while the horizontal components H and D have a strong similarity in the fractal time series, the Z component only sometimes (when it is more influenced by geomagnetic activity) shows the same fractal features of the other two components (see Fig. 4 by Masci and Di Persio, 2012). Bearing in mind these considerations, we should not expect a strong correlation between Kp and the fractal dimension of the Z component for a long time-series duration.…”
Section: Discussionmentioning
confidence: 91%
“…This lack of correlation can be easily explained since the Z component is only weakly influenced by ULF signals induced by solarwind-magnetosphere and magnetosphere-ionosphere interactions. Masci and Di Persio (2012) have shown that, while the horizontal components H and D have a strong similarity in the fractal time series, the Z component only sometimes (when it is more influenced by geomagnetic activity) shows the same fractal features of the other two components (see Fig. 4 by Masci and Di Persio, 2012).…”
Section: Discussionmentioning
confidence: 92%
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“…Because the Earth's crust is fluid saturated, Dahlgren et al (2014) conclude that significant electric currents are not expected to be generated the days before earthquakes during the slow stress accumulation in the region of earthquake nucleation; as a consequence no electric and magnetic signals are expected to be observed on the Earth's surface. Note that studies of data records from the L'Aquila area (see Biagi et al, 2010;Masci, 2012b;Masci and Di Persio, 2012;Masci and De Luca, 2013;Villante et al, 2010) have identified no anomalous magnetic or electric effects during the days or hours before and after the 6 April earthquake that might be hypothesized to have seismogenic origin. Still, in a recent report, Masci and Thomas (2016), by investigating magnetic field measurements from multiple magnetometers and seismic and strong motion records close to the earthquake epicentre, have shown that there is no evidence that might support the generation of an underground electric current in correspondence of the 6 April main shock, when the rupture occurred and the vast majority of mechanical energy was released.…”
Section: On the Hypothesized Generation Mechanismsmentioning
confidence: 99%
“…The study by Masci (2010) demonstrates that the changes of the monofractal characteristics of the geomagnetic field components, which previous reports have claimed to be related to seismogenic signals, were normal disturbances induced by the variation of the global geomagnetic activity level. More recently, Masci and Di Persio (2012) investigate the possible occurrence of seismogenic signals in the magnetic field data from Published by Copernicus Publications on behalf of the European Geosciences Union. 188 F. Masci: On the multi-fractal characteristics of the ULF geomagnetic field the Geomagnetic Observatory of L'Aquila which is located only 6 km from the epicentre of the M w = 6.3 6 April 2009 L'Aquila earthquake.…”
Section: Introductionmentioning
confidence: 99%