Stress tensor inversions along the westernmost North Anatolian Fault Zone and its continuation into the North Aegean Sea
Open Access
- 1 November 2002
- journal article
- research article
- Published by Oxford University Press (OUP) in Geophysical Journal International
- Vol. 151 (2) , 360-376
- https://doi.org/10.1046/j.1365-246x.2002.01753.x
Abstract
No abstract availableKeywords
This publication has 50 references indexed in Scilit:
- Structural characteristics of two strong earthquakes in the North Aegean: ierissos (1932) and Agios Efstratios (1968)Published by Elsevier ,2003
- Kinematics of the Mw=7.2, 12 November 1999, Düzce, Turkey EarthquakeGeophysical Research Letters, 2001
- Surface rupture and rupture mechanism of the October 1, 1995 (Mw=6.2) Dinar earthquake, SW TurkeyTectonophysics, 2000
- Source rupture process of the Kocaeli, Turkey, earthquake of August 17, 1999, obtained by joint inversion of near‐field data and teleseismic dataGeophysical Research Letters, 2000
- Timing, kinematics and cause of Aegean extension: a scenario based on a comparison with simple analogue experimentsPublished by Elsevier ,2000
- Global Positioning System constraints on plate kinematics and dynamics in the eastern Mediterranean and CaucasusJournal of Geophysical Research, 2000
- Microseismicity and focal mechanisms at the western termination of the North Anatolian Fault and their implications for continental tectonicsGeophysical Journal International, 1999
- Stress coupling between earthquakes in northwest Turkey and the north Aegean SeaJournal of Geophysical Research, 1998
- Source inversion of the October 1, 1995, Dinar earthquake (Ms=6.1): a rupture model with implications for seismotectonics in SW TurkeyTectonophysics, 1998
- Seismotectonics of western Anatolia: Regional stress orientation from geophysical and geological dataTectonophysics, 1993