Friction falls towards zero in quartz rock as slip velocity approaches seismic rates
Friction falls towards zero in quartz rock as slip velocity approaches seismic rates
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London: Nature Publishing Group UK
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English
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London: Nature Publishing Group UK
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An important unsolved problem in earthquake mechanics is to determine the resistance to slip on faults in the Earth's crust during earthquakes
1
. Knowledge of coseismic slip resistance is critical for understanding the magnitude of shear-stress reduction and hence the near-fault acceleration that can occur during earthquakes, which affects t...
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Friction falls towards zero in quartz rock as slip velocity approaches seismic rates
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TN_cdi_proquest_miscellaneous_80128245
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_80128245
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ISSN
0028-0836
E-ISSN
1476-4687
DOI
10.1038/nature02249