Skip to main content
Log in

Earthquake science

Shaking faults loose

  • News & Views
  • Published:

From Nature

View current issue Submit your manuscript

Earthquakes often induce aftershocks on other faults, but the mechanisms remain elusive. An innovative analysis tells us more about the effects of dynamic stresses caused by the passage of seismic waves.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Figure 1: The San Francisco Bay area is cut by several large faults, including the San Andreas, which runs through the city of San Francisco, and the Hayward fault east of the bay.

References

  1. Kilb, D., Gomberg, J. & Bodin, P. Nature 408, 570– 574 (2000).

    Article  CAS  Google Scholar 

  2. Hill, D. P. et al. Science 260, 1617– 1623 (1993).

    Article  CAS  Google Scholar 

  3. Stein, R. S. Nature 402, 605–609 ( 1999).

    Article  CAS  Google Scholar 

  4. Harris, R. A. J. Geophys. Res. 103, 24347–24358 (1998).

    Article  Google Scholar 

  5. Marone, C. Annu. Rev. Earth Planet. Sci. 26, 643– 696 (1998).

    Article  CAS  Google Scholar 

  6. Scholz, C. H. Nature 391, 37–42 ( 1998).

    Article  CAS  Google Scholar 

  7. http://www.earthscope.org

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Chris Marone.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Marone, C. Shaking faults loose. Nature 408, 533–535 (2000). https://doi.org/10.1038/35046193

Download citation

  • Issue Date:

  • DOI: https://doi.org/10.1038/35046193

  • Springer Nature Limited

This article is cited by

Navigation