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Failure stress change caused by the 1992 Erzincan Earthquake (Ms=6.8)
Author(s) -
Nalbant Süleyman S.,
Barka A. Aykut,
Alptekin Ömer
Publication year - 1996
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/96gl01323
Subject(s) - aftershock , seismology , north anatolian fault , geology , fault (geology) , fault plane , stress (linguistics) , foreshock , linguistics , philosophy
We calculated Coulomb failure stress change caused by the March 13, 1992 Erzincan, Turkey, earthquake, and explored the relationship between failure stress and the aftershock distribution which includes the Pülümür earthquake (Ms=5.8) that occurred two days later. One of the most significant features of the Erzincan earthquake was the location of aftershocks, which did not correspond with either the eastern segment of the North Anatolian fault zone or the Ovacik fault. This feature can be explained by mapping the failure stress due to the Erzincan earthquake. The map revealed that there is a significant correlation between the aftershock distribution and the areas where static stress was raised by ≥0.3 bar. The 1992 Erzincan earthquake raised the Coulomb failure stress about 1.4 bar at the site of the Pülümür event. This stress rise and optimum orientation of the Pülümür fault favoured its occurrence.