 |
| Titel |
The 11 May 2011 earthquake at Lorca (SE Spain) viewed in a structural-tectonic context |
| VerfasserIn |
R. L. M. Vissers, B. M. L. Meijninger |
| Medientyp |
Artikel
|
| Sprache |
Englisch
|
| ISSN |
1869-9510
|
| Digitales Dokument |
URL |
| Erschienen |
In: Solid Earth ; 2, no. 2 ; Nr. 2, no. 2 (2011-10-05), S.199-204 |
| Datensatznummer |
250000594
|
| Publikation (Nr.) |
copernicus.org/se-2-199-2011.pdf |
|
|
|
|
|
| Zusammenfassung |
| The Lorca earthquake of 11 May 2011 in the Betic Cordillera of SE Spain
occurred almost exactly on the Alhama de Murcia fault, a marked fault that
forms part of a NE-SW trending belt of faults and thrusts. The fault belt is
reminiscent of a strike-slip corridor, but recent structural studies have
provided clear evidence for reverse motions on these faults. Focal
mechanisms of the main earthquake, but also of a foreshock, are strikingly
consistent with structural observations on the Alhama de Murcia fault. This
strengthens the conclusion that, rather than a strike-slip fault, the fault
is at present a contractional fault with an oblique reverse sense of motion,
presumably in response to the NW-directed motion of Africa with respect to
Europe. |
| |
|
| Teil von |
|
|
|
|
|
|
|
|