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• W2617988364 startingPage "5401" @default.
• W2617988364 abstract "Abstract Foreshocks are considered as part of the preparation process for large earthquakes and, as such, can provide important constraints on earthquake generation. We examine the characteristics of the 4 day long foreshock sequence of the 2014 Northern Nagano earthquake ( M w 6.2) using seismograms recorded by a dense seismic observation network including data from a deep borehole closest to the foreshock region. The improved earthquake catalog shows a slow‐speed migration of the sequence toward the main shock hypocenter, implying possible slow‐slip transients which should have caused stress loading at the main shock hypocenter. An analysis of source spectra reveals that foreshocks for M w < 1.5 display a weaker dependence of corner frequency on magnitude than expected for self‐similar scaling, suggesting that these microforeshocks can be regarded as small low‐frequency earthquakes. So far, we might have missed the expected weak low‐frequency preseismic signals, because they emerge only below a certain magnitude and are generally embedded in background noise." @default.
• W2617988364 created "2017-06-05" @default.
• W2617988364 creator A5054182055 @default.
• W2617988364 creator A5061886720 @default.
• W2617988364 date "2017-06-11" @default.
• W2617988364 modified "2023-09-26" @default.
• W2617988364 title "Non-self-similar source property for microforeshocks of the 2014<i>M</i>_<i>w</i>6.2 Northern Nagano, central Japan, earthquake" @default.
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• W2617988364 doi "https://doi.org/10.1002/2017gl073018" @default.
• W2617988364 hasPublicationYear "2017" @default.
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