Ulster University Logo

Ulster Institutional Repository

Failure stress change caused by the 1992 Erzincan earthquake (Ms=6.8)

Biomedical Sciences Research Institute Computer Science Research Institute Environmental Sciences Research Institute Nanotechnology & Advanced Materials Research Institute

Nalbant, SS, Barka, A. A. and Alptekin, O. (1996) Failure stress change caused by the 1992 Erzincan earthquake (Ms=6.8). Geophysical Research Letters, 23 (13). pp. 1561-1564. [Journal article]

This is the latest version of this item.

[img]
Preview
PDF
12Mb

Abstract

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 Pulumur 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 greater than or equal to 0.3 bar. The 1992 Erzincan earthquake raised the Coulomb failure stress about 1.4 bar at the site of the Pulumur event. This stress rise and optimum orientation of the Pulumur fault favoured its occurrence.

Item Type:Journal article
Faculties and Schools:Faculty of Life and Health Sciences
Faculty of Life and Health Sciences > School of Environmental Sciences
Research Institutes and Groups:Environmental Sciences Research Institute
Environmental Sciences Research Institute > Geophysics
ID Code:16863
Deposited By:Dr Suleyman Nalbant
Deposited On:02 Apr 2012 14:29
Last Modified:02 Apr 2012 14:29

Available Versions of this Item

Repository Staff Only: item control page