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) |
|---|---|
| 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