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Foreshock fluctuation and its behaviors
The foreshock region is a turbulent area that forms before a quasi-parallel shock. It is caused by the interaction between reflected particles from the bow shock and oncoming waves in the solar wind. Typically, the foreshock is located on the dawn side.Gilbert Pi +2 more
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Real-time discrimination of earthquake foreshocks and aftershocks
Nature, 2019Laura Gulia, Stefan Wiemer
exaly
Nucleation of the 1999 Izmit earthquake by a triggered cascade of foreshocks
Nature Geoscience, 2018William Ellsworth, Fatih Bulut
exaly
Seismic Amplitude Measurements Suggest Foreshocks Have Different Focal Mechanisms than Aftershocks
Science, 1978Gary S Fuis
exaly
Foreshocks explained by cascades of triggered seismicity
Journal of Geophysical Research, 2003Agnès Helmstetter, Didier Sornette
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