Abstract
The dynamics of the tectonic faults that produce earthquakes remain puzzling. An inference from laboratory experiments could help: at high rates of slip, friction at the interface may fall dramatically.
Original language | English (US) |
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Pages (from-to) | 405-406 |
Number of pages | 2 |
Journal | Nature |
Volume | 427 |
Issue number | 6973 |
DOIs | |
State | Published - Jan 29 2004 |
All Science Journal Classification (ASJC) codes
- General