Uplift and subsidence from oblique slip: the Ganos–Marmara bend of the North Anatolian Transform, western Turkey
- 18 September 2004
- journal article
- Published by Elsevier in Tectonophysics
- Vol. 391 (1-4), 239-258
- https://doi.org/10.1016/j.tecto.2004.07.015
Abstract
No abstract availableKeywords
This publication has 43 references indexed in Scilit:
- Investigation of the tectonics of the Main Marmara Fault by means of deep-towed seismic dataTectonophysics, 2002
- Exploring submarine earthquake geology in the Marmara SeaEos, 2002
- Active faults and evolving strike-slip basins in the Marmara Sea, northwest Turkey: a multichannel seismic reflection studyTectonophysics, 2000
- Investigation of the submarine active tectonism in the Gulf of Gökova, southwest Anatolia–southeast Aegean Sea, by multi-channel seismic reflection dataTectonophysics, 1999
- An active, deep marine strike‐slip basin along the North Anatolian fault in TurkeyTectonics, 1999
- Global Positioning System measurements of present‐day crustal movements in the Arabia‐Africa‐Eurasia plate collision zoneJournal of Geophysical Research, 1997
- Origin of the Sea of Marmara as Deduced from Neogene to Quaternary Paleogeographic Evolution of its FrameInternational Geology Review, 1997
- Deformation around stepovers in strike-slip fault zonesJournal of Structural Geology, 1995
- The Sea of Marmara: a plate boundary sea in an escape tectonic regimeTectonophysics, 1995
- Tethyan evolution of Turkey: A plate tectonic approachTectonophysics, 1981