The Spitak (Armenia) earthquake of 7 December 1988: field observations, seismology and tectonics
Abstract
The epicentre of the destructive earthquake that devastated northern Armenia, the strongest in the region since historical times, is located within the Lesser Caucasus, a mountain country subjected to north-south compression by the push of the Arabian plate. A French-Soviet field expedition studied surface breaks and aftershock activity. The fault scarp could be followed for 13 kilometres and showed a reverse dislocation of 1.6 metres. Aftershocks are shallower than 13 kilometres, and delimit a ruptured surface of about 300km2.
- Publication:
-
Nature
- Pub Date:
- June 1989
- DOI:
- 10.1038/339675a0
- Bibcode:
- 1989Natur.339..675C