Creep events slip less than ordinary earthquakes

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Creep events slip less than ordinary earthquakes

[1] We find that slow seismic events have smaller fault slips compared to ordinary earthquakes with similar dimensions. For ordinary earthquakes, the ratio of slip to fault length is largely consistent, yet the physical controls on this ratio are unknown. Recently discovered slow slip or creep events in which faults move quasi-statically over periods of days to years shed new light on this old ...

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ژورنال

عنوان ژورنال: Geophysical Research Letters

سال: 2007

ISSN: 0094-8276

DOI: 10.1029/2007gl030917