Repeating earthquakes and interplate coupling along the western part of the North Anatolian Fault
Author:
Funder
Japan Society for the Promotion of Science
Japan Science and Technology Agency
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geophysics
Reference42 articles.
1. Rupture characteristics of the A.D. 1912 Mürefte (Ganos) earthquake segment of the North Anatolian fault (western Turkey);Aksoy;Geology,2010
2. The seismic activity of the Marmara Sea region over the last 2000 years;Ambraseys;Bull. Seismol. Soc. Am.,2002
3. Asymmetric slip partitioning in the Sea of Marmara pull-apart: a clue to propagation processes of the North Anatolian Fault?;Armijo;Terra Nova,2002
4. The surface rupture and slip distribution of the 17 August 1999 Izmit earthquake (M 7.4), North Anatolian fault;Barka;Bull. Seismol. Soc. Am.,2002
5. A simple stick-slip and creep-slip model for repeating earthquakes and its implication for microearthquakes at Parkfield;Beeler;Bull. Seismol. Soc. Am.,2001
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2. Spatio-temporal variations of seismic coupling along a transform fault: the western North Anatolian Fault Zone;Geophysical Journal International;2023-07-27
3. Variation of Fault Creep Along the Overdue Istanbul‐Marmara Seismic Gap in NW Türkiye;Geophysical Research Letters;2023-03-22
4. Prevalence of Repeating Earthquakes in the Continental Crust and Subducting Slabs: Triggering of Earthquakes by Aseismic Slip;Journal of Geophysical Research: Solid Earth;2023-02
5. Evaluation of current earthquake activity on the Ganos Fault: MONGAN network test analysis;Bulletin Of The Mineral Research and Exploration;2022-06-30
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