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Dynamic triggering of fault slip

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Abstract

Earthquakes and rock bursts belong to those natural phenomena which pose a great threat to mankind and they have been associated with mythicism for a long time. In fact, even today with all the computer capabilities man has at his/her disposal there are more questions to be asked than satisfying answers available. In fact, it is not at all clear how earthquakes can be triggered and what kind of connection there exists between an earthquake and the earth’s geological structure.

Keywords

Stress Wave Blast Wave Rock Burst Fault Slip Rayleigh Surface Wave 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Gilbert, G.K. (1884). A theory of earthquakes of the Great Basin with a practical application. Am. J. Sci. 27. pp 49–54.CrossRefGoogle Scholar
  2. Mandl, G. (1988). Mechanics of tectonic faulting. Elsevier.Google Scholar
  3. Scholz, C.H. (1990). The mechanics of earthquakes and faulting. Cambridge University Press.Google Scholar
  4. SWIFD-FD Program (1995). Fracture and Photomechanics Laboratory, Institute of Mechanics, Technical University Vienna.Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2000

Authors and Affiliations

  1. 1.Institute of MechanicsTechnical University ViennaViennaAustria

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