Abstract
The mechanics of great subduction earthquakes are influenced by the frictional properties, structure, and composition of the plate-boundary fault. We present observations of the structure and composition of the shallow source fault of the 2011 Tohoku-Oki earthquake and tsunami from boreholes drilled by the Integrated Ocean Drilling Program Expedition 343 and 343T. Logging-while-drilling and core-sample observations show a single major plate-boundary fault accommodated the large slip of the Tohoku-Oki earthquake rupture, as well as nearly all the cumulative interplate motion at the drill site. The localization of deformation onto a limited thickness (less than 5 meters) of pelagic clay is the defining characteristic of the shallow earthquake fault, suggesting that the pelagic clay may be a regionally important control on tsunamigenic earthquakes.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 1208-1211 |
| Number of pages | 4 |
| Journal | Science |
| Volume | 342 |
| Issue number | 6163 |
| DOIs | |
| State | Published - 2013 |
| Externally published | Yes |
ASJC Scopus subject areas
- General