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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
openaire   +1 more source

Foreshocks and Their Potential Deviation from General Seismicity

Bulletin of The Seismological Society of America (BSSA), 2018
S. Seif   +4 more
semanticscholar   +1 more source

Statistical Features of Foreshocks in Instrumental and ETAS Catalogs

Pure and Applied Geophysics, 2017
E. Lippiello   +4 more
semanticscholar   +1 more source

Diversity of the 2014 Iquique’s foreshocks and aftershocks: clues about the complex rupture process of a Mw 8.1 earthquake

Journal of Seismology, 2016
S. León‐Ríos   +5 more
semanticscholar   +1 more source

Short-Term Foreshocks and Earthquake Prediction

Pre-Earthquake Processes, 2018
G. Papadopoulos   +2 more
semanticscholar   +1 more source

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