Kinematic consistency between the Dead Sea Fault Zone and the Neogene and Quaternary left-lateral faulting in SE Turkey
- 8 October 2004
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 391 (1-4), 203-237
- https://doi.org/10.1016/j.tecto.2004.07.014
Abstract
No abstract availableKeywords
This publication has 50 references indexed in Scilit:
- Rate of strike-slip motion on the Amanos Fault (Karasu Valley, southern Turkey) constrained by K–Ar dating and geochemical analysis of Quaternary basaltsTectonophysics, 2002
- Deformation around stepovers in strike-slip fault zonesJournal of Structural Geology, 1995
- Architecture of late orogenic Quaternary basins in northeastern Mediterranean SeaTectonophysics, 1992
- The Dead Sea transform fault systemTectonophysics, 1990
- The structural relationship between the East Anatolian and Dead Sea fault zones in southeastern TurkeyTectonophysics, 1990
- Observations on the complexity of the east anatolian fault, turkeyJournal of Structural Geology, 1987
- Variation of slip and creep along the levant rift over the past 4500 yearsTectonophysics, 1981
- Internal structure of the Dead Sea leaky transform (rift) in relation to plate kinematicsTectonophysics, 1981
- The tectonic development of the western margin of the Gulf of Elat (Aqaba) riftTectonophysics, 1981
- Tectonic significance of mesofracture systems associated with the Lebanese segment of the Dead Sea transform faultJournal of Structural Geology, 1979