| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4687974 | Journal of Geodynamics | 2015 | 74 Pages |
Abstract
The first weeks following the megatrust Mw = 8.8 Maule earthquake in 2010 were characterized by a sudden increase of the outer rise seismic activity, located between 34° S and 35°30â²Â S. We concluded that this phenomenon is a result of an intensification of the water infiltration process in the outer rise, presumably triggered by the main shock, whose epicenter was located some 100 km to the south east of the cluster.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
E. Moscoso, I. Grevemeyer,