Stress coupling between earthquakes in northwest Turkey and the north Aegean Sea
- 10 October 1998
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 103 (B10) , 24469-24486
- https://doi.org/10.1029/98jb01491
Abstract
No abstract availableKeywords
This publication has 56 references indexed in Scilit:
- Some characteristic features of the Anatolian fault zonePublished by Elsevier ,2003
- Structural characteristics of two strong earthquakes in the North Aegean: ierissos (1932) and Agios Efstratios (1968)Published by Elsevier ,2003
- Seismic activity triggered by stress changes after the 1978 events in the Asal Rift, DjiboutiGeophysical Research Letters, 1996
- Failure stress change caused by the 1992 Erzincan Earthquake (Ms=6.8)Geophysical Research Letters, 1996
- In the shadow of 1857‐the effect of the Great Ft. Tejon Earthquake on subsequent earthquakes in southern CaliforniaGeophysical Research Letters, 1996
- The Sea of Marmara: a plate boundary sea in an escape tectonic regimeTectonophysics, 1995
- Seismotectonics of western Anatolia: Regional stress orientation from geophysical and geological dataTectonophysics, 1993
- Neogene evolution of the Denizli region of western TurkeyJournal of Structural Geology, 1993
- Structural Control of Flank Volcanism in Continental RiftsScience, 1991
- Analyses of fault mechanisms and expansion of southwestern Anatolia since the late MioceneTectonophysics, 1981