Forensic seismology

From Wikipedia, the free encyclopedia

Forensic seismology is the forensic use of the techniques of seismology to detect and study distant phenomena, particularly explosions, including those of nuclear weapons.[1]

Because of the efficiency with which seismic waves propagate through the Earth and the technical difficulties of decoupling explosions to diminish their seismic radiation, forensic seismology is a critical technique in the enforcement of bans on underground nuclear testing.[2]

In addition to nuclear explosions, the signatures of many other kinds of explosions can also be detected and analyzed by forensic seismology,[1] and even other phenomena such as ocean waves (the global microseism), the movement of icebergs across the sea floor or in collision with other icebergs, or explosions within submarines.[3][4]

Organizations with expertise in forensic seismology include AWE Blacknest, Los Alamos National Laboratory, Sandia National Laboratory, and Lawrence Livermore National Laboratory.

See also

References

  1. ↑ 1.0 1.1 J. David Rogers and Keith D. Koper. "Some Practical Applications of Forensic Seismology". Retrieved 2011-09-09. 
  2. ↑ John J. Zucca (September 1998). "Forensic Seismology Supports CTBT". Lawrence Livermore National Laboratory. Retrieved 2011-09-09. 
  3. ↑ Richard A. Lovett (5 March 2009). "Forensic seismology". COSMOS magazine. 
  4. ↑ Christina Reed (February 2001). "Sinking the Kursk". GeoTimes. Retrieved 2011-09-09. 
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