Reply: Characteristic features of the North Anatolian Fault in the Eastern Marmara Region and its tectonic evolution

Marine Geology

Volumn 194, Issue 3-4, 2003, Pages 203-208

  Alpar, Bedri ^a   Yaltirak, Cenk ^b  

^a ISTANBUL UNIVERSITY   (Turkey)

^b ISTANBUL TECHNICAL UNIVERSITY   (Turkey)

Author keywords

[No Author keywords available]

Indexed keywords

TECTONIC EVOLUTION;

EID: 0037445436     PISSN: 00253227     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0025-3227(02)00707-7     Document Type: Note

References (9)

1. Aksu, A.E., Calon, T.J., Hiscott, R.N., Yaşar, D., 2000. Anatomy of the North Anatolian fault zone in the Marmara Sea, Western Turkey: Extensional basins above a continental transform. GSA Today 10, 1-2.
2. Alpar, B., Yaltirak, C., 2002. Characteristic features of the North Anatolian Fault in the Eastern Marmara Region and its tectonic evolution. Mar. Geol. 190, 329-350.
3. rd Workshop, 4-5 November 1999, Cumhuriyet University, Sivas, Abstract Book, p. 9.
4. Gokaşan, E., Alpar, B., Gazioglu, C., Yucel, Z.Y., Tok, B., Dogan, E., Guneysu, C., 2001. Active tectonics of the İzmit Gulf (NE Marmara Sea): from high resolution seismic and multi-beam bathymetry data. Mar. Geol. 175, 273-296.
5. Yaltirak, C., 2002. Tectonic evolution of the Marmara Sea and its surroundings. Mar. Geol. 190, 493-529.
6. Yaltirak, C., Alpar, B., 2002a. Evolution of the middle strand of North Anatolian fault and shallow seismic investigation of the Southestern Marmara Sea (Gemlik Bay). Mar. Geol. 190, 307-327.
7. Yaltirak, C., Alpar, B., 2002b. Kinematics and evolution of the Northern branch of the North Anatolian fault (Ganos Fault) between the Sea of Marmara and the Gulf of Saros. Mar. Geol. 190, 351-366.
8. Yaltirak, C., Alpar, B., Sakinç, M., Yüce, H., 2000. Origin of the Strait of Çanakkale (Dardanelles): regional tectonics and the Mediterranean-Marmara incursion. Mar. Geol. 164, 139-156.
9. Yaltirak, C., Sakinç, M., Aksu, A.E., Hiscott, R., Galleb, B., Ülgen, U.B., 2002. Late Pleistocene uplift history along southwestern Marmara Sea determined from raised coastal deposits and global sea level variations. Mar. Geol. 190, 283-305.