Seismogenic layer

In

aseismic zone where ductile creep becomes the dominant process. The location of this change in deformation style is sometimes referred to as the brittle–ductile transition zone.^[4]

References

ISBN 9780521655408
. Retrieved June 12, 2012.

doi:10.1016/S0012-821X(03)00289-9
.

^ Hayes, Gavin; Crone, Tony. "At what depth do earthquakes occur? What is the significance of the depth?". USGS.gov.

^ Cole, J.; Hacker, B.; Ratschbacher, L.; Dolan, J.; Seward, G.; Frost, E.; Frank, W. (2007). "Localized ductile shear below the seismogenic zone: Structural analysis of an exhumed strike-slip fault, Austrian Alps" (PDF). Journal of Geophysical Research. 112 (B12): B12304.
doi:10.1029/2007JB004975
.

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Retrieved from "https://en.wikipedia.org/w/index.php?title=Seismogenic_layer&oldid=1156583872"

[Initiated-1] ISBN 9780521655408
. Retrieved June 12, 2012.

[2] :10.1016/S0012-821X(03)00289-9
.

[3] Hayes, Gavin; Crone, Tony. "At what depth do earthquakes occur? What is the significance of the depth?". USGS.gov.

[Ductile-4] Cole, J.; Hacker, B.; Ratschbacher, L.; Dolan, J.; Seward, G.; Frost, E.; Frank, W. (2007). "Localized ductile shear below the seismogenic zone: Structural analysis of an exhumed strike-slip fault, Austrian Alps" (PDF). Journal of Geophysical Research. 112 (B12): B12304.
doi:10.1029/2007JB004975
.

[4]