Monitoring aseismic surface creep along the North Anatolian Fault (Turkey) using ground-based LIDAR

V. Karabacak*, E. Altunel, Z. Cakir

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

42 Citations (Scopus)

Abstract

We studied the surface creep along the North Anatolian Fault (NAF), one of the most seismically active structures of the eastern Mediterranean, by using a ground-based light detection and ranging (LIDAR) system at the Ismetpasa and Destek sections. Aseismic surface creep has been known to exist at Ismetpasa since the 1970s, but it has not been previously reported for the Destek site. Three manmade walls across the fault were monitored for 3. yrs between June 2007 and November 2009 using LIDAR. The surveys revealed that a significant amount of aseismic strain is being continuously released along these sections of the NAF: 6.8-10.0 ± 4.0. mm/yr and 9.1-10.1 ± 4.0. mm/yr at two sites near Ismetpasa and 6.0-7.2 ± 4.0. mm/yr at Destek. Despite this, these fault segments are still capable of generating large earthquakes since 50-70% of the yearly slip (i.e., 20-25. mm/yr) still accumulates on the fault, as was demonstrated by the well-known 20th century earthquake sequence of 1939-1999.

Original languageEnglish
Pages (from-to)64-70
Number of pages7
JournalEarth and Planetary Science Letters
Volume304
Issue number1-2
DOIs
Publication statusPublished - 1 Apr 2011

Funding

This research was supported by the Eskisehir Osmangazi University Research Foundation ( 200615006 and 200615026 ). The authors are grateful to Mr. Önder Yönlü for his assistance in the field. Thanks go to R. Bengü Karabacak for her help on statistical computations. The authors are grateful for the helpful comments and constructive reviews by three anonymous reviewers which improved the manuscript.

FundersFunder number
Eskisehir Osmangazi University Research Foundation200615006, 200615026

    Keywords

    • Aseismic surface slip
    • Creep
    • Light detection and ranging (LIDAR)
    • North Anatolian Fault

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