Land-level changes produced by the M-w 8.8 2010 Chilean earthquake
- We observed vertically displaced coastal and river markers after the 27 February 2010 Chilean earthquake [moment magnitude (Mw) 8.8]. Land-level changes range between 2.5 and -1 meters, evident along an ~500-kilometers- long segment identified here as the maximum length of coseismic rupture. A hinge line located 120 kilometers from the trench separates uplifted areas, to the west, from subsided regions. A simple elastic dislocation model fits these observations well; model parameters give a similar seismic moment to seismological estimates and suggest that most of the plate convergence since the 1835 great earthquake was elastically stored and then released during this event.
| Verfasserangaben: | Marcelo Farïas, Gabriel Vargas, Andrés Tassara, Sébastien Carretier, Stéphane Baize, Daniel MelnickORCiDGND, Klaus Bataille |
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| URL: | http://www.sciencemag.org/ |
| DOI: | https://doi.org/10.1126/science.1192094 |
| ISSN: | 0036-8075 |
| Publikationstyp: | Wissenschaftlicher Artikel |
| Sprache: | Englisch |
| Jahr der Erstveröffentlichung: | 2010 |
| Erscheinungsjahr: | 2010 |
| Datum der Freischaltung: | 25.03.2017 |
| Quelle: | Science. - ISSN 0036-8075. - 329 (2010), 5994, S. 916 |
| Organisationseinheiten: | Mathematisch-Naturwissenschaftliche Fakultät / Institut für Geowissenschaften |
| Peer Review: | Referiert |
| Name der Einrichtung zum Zeitpunkt der Publikation: | Mathematisch-Naturwissenschaftliche Fakultät / Institut für Erd- und Umweltwissenschaften |
