A Supershear Transition Mechanism for Cracks

Seismic data indicate that fault ruptures follow complicated paths with variable velocity because of inhomogeneities in initial stress or fracture energy. We report a phenomenon unique to three-dimensional cracks: Locally stronger fault sections, rather than slowing ruptures, drive them forward at v...

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Veröffentlicht in:Science (American Association for the Advancement of Science) 2003-03, Vol.299 (5612), p.1557-1559
Hauptverfasser: Dunham, Eric M., Favreau, Pascal, Carlson, J. M.
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Favreau, Pascal
Carlson, J. M.
description Seismic data indicate that fault ruptures follow complicated paths with variable velocity because of inhomogeneities in initial stress or fracture energy. We report a phenomenon unique to three-dimensional cracks: Locally stronger fault sections, rather than slowing ruptures, drive them forward at velocities exceeding the shear wave speed. This supershear mechanism differentiates barrier and asperity models of fault heterogeneity, which previously have been regarded as indistinguishable. High strength barriers concentrate energy, producing potentially destructive pulses of strong ground motion.
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subjects Earth sciences
Earth, ocean, space
Earthquakes
Earthquakes, seismology
Energy
Exact sciences and technology
Faults (Geology)
Fracture mechanics
France
Internal geophysics
Kinetics
Laboratory Experiments
Materials science
Mechanical properties
Motion
Seismology
Shear (Mechanics)
Speed
Tectonics. Structural geology. Plate tectonics
United States
Velocity
title A Supershear Transition Mechanism for Cracks
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