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 |
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creator | Dunham, Eric M. 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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High strength barriers concentrate energy, producing potentially destructive pulses of strong ground motion.</description><identifier>ISSN: 0036-8075</identifier><identifier>EISSN: 1095-9203</identifier><identifier>DOI: 10.1126/science.1080650</identifier><identifier>PMID: 12624262</identifier><identifier>CODEN: SCIEAS</identifier><language>eng</language><publisher>Washington, DC: American Association for the Advancement of Science</publisher><subject>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. 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M.</creatorcontrib><title>A Supershear Transition Mechanism for Cracks</title><title>Science (American Association for the Advancement of Science)</title><addtitle>Science</addtitle><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.</description><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Earthquakes</subject><subject>Earthquakes, seismology</subject><subject>Energy</subject><subject>Exact sciences and technology</subject><subject>Faults (Geology)</subject><subject>Fracture mechanics</subject><subject>France</subject><subject>Internal geophysics</subject><subject>Kinetics</subject><subject>Laboratory Experiments</subject><subject>Materials science</subject><subject>Mechanical properties</subject><subject>Motion</subject><subject>Seismology</subject><subject>Shear (Mechanics)</subject><subject>Speed</subject><subject>Tectonics. Structural geology. 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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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