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PROGRESSIVE FAILURE ON THE NORTH ANATOLIAN FAULT SINCE 1939 BYEARTHQUAKE STRESS TRIGGERING (1997)

Ten M>=6.7 earthquakes ruptured 1,000 km of the North Anatolian fault (Turkey) during 1939-92, providing an unsurpassed opportunity to study how one large shock sets up the next. Weuse the mapped surface slip and fault geometry to infer the transfer of stress throughout thesequence
Reference:
Geophysical Journal International,1997, VOL 128, pp 594-604
Organization:
U.S. Geological Survey, MS 977, Menlo Park, CA 94025 USA
Turkey
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