Rupture mechanism and interface separation in foam rubber models of earthquakes: a possible solution to the heat flow paradox and the paradox of large overthrusts

Tectonophysics

Volumn 218, Issue 1-3, 1993, Pages 59-67

  Brune, James N ^a   Brown, Stephen ^b   Johnson, Peggy A ^a  

^a UNIVERSITY OF NEVADA   (United States)

^b SANDIA NATIONAL LABORATORIES   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

EARTHQUAKE; FOAM RUBBER MODEL; HEAT FLOW; OVERTHRUST; RUPTURE MECHANISM; STICK-SLIP;

EID: 0027382646     PISSN: 00401951     EISSN: None     Source Type: Journal    
DOI: 10.1016/0040-1951(93)90259-M     Document Type: Article

References (62)

1. Strong ground motion and source mechanism of the Mexico earthquake of Sept. 19, 1985
2. Foam rubber modeling of the El Centro terminal substation building
3. Surface strong motion associated with a stick-slip event in a foam rubber model of earthquakes
4. Rubber friction and rheology of viscoelastic contact
5. A source theory for complex earthquakes
6. The friction-speed relation and its influence on the critical velocity of stick-slip motion
7. The area of contact between stationary and between moving surfaces
8. Stick-slip as a mechanism for earthquakes
9. Tectonic stress and the spectra of seismic shear waves from earthquakes
10. Earthquake modeling by stick-slip along precut surfaces in stressed foam rubber
11. The physics of earthquake strong motion
12. Seismic source dynamics, radiation and stress
13. Heat flow stress and rate of slip along the San Andreas Fault California
14. Low stress-drop earthquakes in the light of new data from the Anza, California, telemetered digital array
15. Constitutive relations for foam rubber stick-slip
16. Nucleation, predictability, and rupture mechanism in foam rubber models of earthquakes
17. The mechanics of stick-slip
18. P/S spectra ratios from the Guerrero accelerograph array and Oaxaca aftershocks
19. Origin of high P/S spectra ratios from the Guerrero accelerograph array and Oaxaca aftershocks
20. Elastic interface waves involving separation
21. Can two solids slide without slipping?
22. Elastic interface waves and sliding between two solids
23. Time-dependent friction and the mechanics of stick-slip
24. A model for the nucleation of earthquake slip
25. Discussion
26. The corner frequency shift earthquake source models and Q
27. Rupture propagation and focusing of energy in a foam rubber model of a stick-slip earthquake
28. Total energy and energy spectral density of elastic wave radiation from propagating faults
29. Hydraulic fracturing in situ stress measurements to 2.1 km depth at Cajon Pass, California
30. Evidence for and implications of selfhealing pulses of slip in earthquake rupture
31. Heat flow near major strike-slip faults in California
32. Properties of strong-motion earthquakes
33. Focal mechanisms and the state of stress on the San Andreas fault in Southern California
34. The stress heat-flow paradox and thermal results from Cajon Pass
35. Heat flow from Cajon Pass, Fault strength, and tectonic implications
36. Model for steady-state friction
37. Acoustic fluidization: A new geological process?
38. Corner frequencies of P and S waves and models of earthquake sources
39. State of stress near the San Andreas Fault: implications for wrench tectonics
40. Models and computational methods for dynamic friction phenomena
41. Know your faults
42. Fault plane solutions for the 1984 Morgan Hill, California, earthquake sequence: evidence for the state of stress on the Calaveras fault
43. max
44. A specific barrier model for the quantitative description of inhomogeneous faulting and the prediction of strong ground motion. Part II. Applications of the model
45. The mechanical paradox of large overthrusts
46. Dynamic stress drop and rupture dynamics of the Oct. 15, 1979 Imperial Valley, CA earthquake
47. A study of the stick-slip process
48. Friction laws and instabilities: A quasistatic analysis of some dry frictional behavior
49. Slip instability and state variable friction laws
50. How does rubber slide?
51. The critical slip distance for seismic faulting
52. Mechanics of faulting
53. In situ stress orientation near the San Andreas fault: preliminary results to 2.1 km depth from the Cajon Pass scientific drillhole
54. Significance of the normal degree of freedom and natural normal vibrations in contact friction
55. The squeeze film under boundary lubrication conditions and its effect on the vertical displacement of sliding bodies
56. P/S spectral ratios for the Anza array: evidence for normal motions during fault rupture
57. The spectra of seismic radiation from a tensile crack
58. Triggered slip along the San Andreas fault after the 8 July 1986 North Palm Springs Earthquake
59. Heat flow and seduction in southern Mexico
60. In situ stress measurements to 35 km depth in the Cajon pass scientific research borehole implications for the mechanics of crustal faulting
61. New evidence on the state of stress of the San Andreas Fault system
62. The Cajon pass scientific drilling experiment: overview of phase I