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MICROSEISMICITY AND FOCAL MECHANISMS AT THE WESTERN TERMINATION OF THE NORTH ANATOLIAN FAULT AND THEIR IMPLICATIONS FOR CONTINENTALTECTONICS (1999)

For seven weeks, a temporary network of 68 seismological stations was operated in Central Greece, in the region of Thessaly and Evia, located at the western termination of the North Anatolian Fault system. We recorded 510 earthquakes and computed 80 focal mechanisms.
Reference:
Geophys. J. Int. (1999) 137, 891-908
Organization:
Laboratoire de Geophysique Interne et T ectonophysique, IRIGM-CNRS, BPP53X, 38041 Grenoble Cedex 9, France.
Greece
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