Seismic moment

Seismic momentis a quantity used byseismologiststo measure the size of anearthquake.The scalar seismic moment$M_{0}$is defined by the equation $M_{0}=\mu AD$,where

• $\mu$is theshear modulusof the rocks involved in the earthquake (inpascals(Pa), i.e. newtons per square meter)
• $A$is the area of the rupture along thegeologic faultwhere the earthquake occurred (in square meters), and
• $D$is the average slip (displacement offset between the two sides of the fault) on$A$(in meters).

$M_{0}$thus has dimensions oftorque,measured innewton meters.The connection between seismic moment and a torque is natural in the body-force equivalent representation of seismic sources as adouble-couple(a pair of force couples with opposite torques): the seismic moment is the torque of each of the two couples. Despite having the same dimensions as energy, seismic moment is not a measure of energy. Therelations between seismic moment, potential energy drop and radiated energyare indirect and approximative.

The seismic moment of an earthquake is typically estimated using whatever information is available to constrain its factors. For modern earthquakes, moment is usually estimated fromground motionrecordings of earthquakes known asseismograms.For earthquakes that occurred in times before modern instruments were available, moment may be estimated from geologic estimates of the size of the fault rupture and the slip.

Seismic moment is the basis of themoment magnitude scaleintroduced by Caltech'sThomas C. HanksandHiroo Kanamori,which is often used to compare the size of different earthquakes and is especially useful for comparing the sizes of large (great) earthquakes.

The seismic moment is not restricted to earthquakes. For a more general seismic source described by a seismic moment tensor$M_{ij}$(a symmetric tensor, but not necessarily a double couple tensor), the seismic moment is

$M_{0}={\frac {1}{\sqrt {2}}}(M_{ij}^{2})^{1/2}$

See also

• Richter magnitude scale
• Moment magnitude scale

Sources

• Aki, Keiiti(1966),"Generation and propagation of G waves from the Niigata earthquake of June 14, 1964. Part 2. Estimation of earthquake moment, released energy and stress-strain drop from G wave spectrum"(PDF),Bulletin of the Earthquake Research Institute,44:73–88.

• Aki, Keiiti; Richards, Paul G. (2002),Quantitative seismology(2 ed.), University Science Books,ISBN0-935702-96-2.

• Fowler, C. M. R.(1990),The Solid Earth,Cambridge, UK: Cambridge University Press,ISBN0-521-38590-3.

• Udías, Agustín (1991), "Source Mechanism of Earthquakes",Advances in Geophysics,33:81–140,Bibcode:1991AdGeo..33...81U,doi:10.1016/S0065-2687(08)60441-0,ISBN9780120188338.