Role of stress triggering in earthquake migration on the North Anatolian fault

Physics and Chemistry of the Earth
By: , and 



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. Calculations of the change in Coulomb failure stress reveal that 9 out of 10 ruptures were brought closer to failure by the preceding shocks, typically by 5 bars, equivalent to 20 years of secular stressing. We translate the calculated stress changes into earthquake probabilities using an earthquake-nucleation constitutive relation, which includes both permanent and transient stress effects. For the typical 10-year period between triggering and subsequent rupturing shocks in the Anatolia sequence, the stress changes yield an average three-fold gain in the ensuing earthquake probability. Stress is now calculated to be high at several isolated sites along the fault. During the next 30 years, we estimate a 15% probability of a M???6.7 earthquake east of the major eastern center of Erzincan, and a 12% probability for a large event south of the major western port city of Izmit. Such stress-based probability calculations may thus be useful to assess and update earthquake hazards elsewhere. ?? 1997 Elsevier Science Ltd.

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Role of stress triggering in earthquake migration on the North Anatolian fault
Series title Physics and Chemistry of the Earth
DOI 10.1016/S0079-1946(97)00039-6
Volume 21
Issue 4
Year Published 1996
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Physics and Chemistry of the Earth
First page 225
Last page 230
Google Analytic Metrics Metrics page
Additional metadata about this publication, not found in other parts of the page is in this table