Spring and Block Model

Quantity:

    • 1

Courses:

    • GEOS1034: Hazards

Used to Teach About:


USING THE SPRING-BLOCK MODEL WITH THE VERNIER WIRELESS DYNAMIC SENSORS

References:

  • Burridge, R., & Knopoff, L. (1967). Model and theoretical seismicity. Bulletin of the seismological society of america, 57(3), 341-371.

  • Di Toro, G., Goldsby, D. L., & Tullis, T. E. (2004). Friction falls towards zero in quartz rock as slip velocity approaches seismic rates. Nature, 427(6973), 436.

  • Handy, M. R., Hirth, G., & Bürgmann, R. (2007). Continental fault structure and rheology from the frictional-to-viscous transition downward. Tectonic Faults: Agents of Change on a Dynamic Earth, 139-81.

  • Moore, D. E., & Rymer, M. J. (2007). Talc-bearing serpentinite and the creeping section of the San Andreas fault. Nature, 448(7155), 795.

  • Rice, J. R., & Cocco, M. (2007). Seismic fault rheology and earthquake dynamics. Tectonic Faults: Agents of Change on a Dynamic Earth, 99-137.

  • Scholz, C. H. (1998). Earthquakes and friction laws. Nature, 391(6662), 37. https://www.nature.com/articles/34097

  • Scholz, C. H. (2002). The Mechanics of Earthquakes and Faulting. The Mechanics of Earthquakes and Faulting, by Christopher H. Scholz, pp. 496. ISBN 0521652235. Cambridge, UK: Cambridge University Press, June 2002., 496.

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