Theory of time-dependent rupture in the Earth

Das, S.; Scholz, C H

doi:10.1029/JB086iB07p06039

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Theory of time-dependent rupture in the Earth

Author(s): S. Das , C. H. Scholz

Publication date Created: July 10 1981

Publication date (Print): July 10 1981

Journal: Journal of Geophysical Research: Solid Earth

Publisher: American Geophysical Union (AGU)

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Most cited references 33

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Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan

Masataka Ando (1975)

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Mechanism of tsunami earthquakes

Hiroo Kanamori (1972)

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Aftershocks caused by pore fluid flow?

Y A Nur, J R Booker (1972)

Large shallow earthquakes can induce changes in the fluid pore pressure that are comparable to stress drops on faults. The subsequent redistribution of pore pressure as a result of fluid flow slowly decreases the strength of rock and may result in delayed fracture. The agreement between computed rates of decay and observed rates of aftershock activity suggests that this is an attractive mechanism for aftershockss.