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A. Nikishin, M. Korotaev, A. Ershov, M. Brunet (2003)
The Black Sea basin: tectonic history and Neogene–Quaternary rapid subsidence modellingSedimentary Geology, 156
Colin Cotter, David Ham, Christopher Pain (2008)
A mixed discontinuous/continuous finite element pair for shallow-water ocean modellingOcean Modelling, 26
N. Görür (1988)
Timing of opening of the Black Sea basinTectonophysics, 147
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I. Kuşçu, J. Parke, R. White, D. McKenzie, G. Anderson, T. Minshull, N. Görür, A. Şengör (2004)
ACTIVE SLUMPING OFFSHORE AMASRA (SOUTHWEST BLACK SEA) AND ITS RELATION WITH REGIONAL TECTONICSBulletin of the mineral research and exploration, 128
Y. Altınok, S. Ersoy (2000)
Tsunamis Observed on and Near the Turkish CoastNatural Hazards, 21
L. Zonenshain, X. Pichon (1986)
Deep basins of the Black Sea and Caspian Sea as remnants of Mesozoic back-arc basinsTectonophysics, 123
C. Cotter, D. Ham (2010)
Numerical wave propagation for the triangular P1DG-P2 finite element pairJ. Comput. Phys., 230
A. Şengör (1979)
The North Anatolian transform fault: its age, offset and tectonic significanceJournal of the Geological Society, 136
A. Robinson (1997)
Regional and Petroleum Geology of the Black Sea and Surrounding Region
A. Okay, A. Şengör, N. Görür (1994)
Kinematic history of the opening of the Black Sea and its effect on the surrounding regionsGeology, 22
A. Şengör, N. Görür, F. Şaroǧlu (1985)
Strike-Slip Faulting and Related Basin Formation in Zones of Tectonic Escape: Turkey as a Case Study
A. Şengör, N. Canitez (2013)
The North Anatolian Fault
D. McKenzie (1972)
Active Tectonics of the Mediterranean RegionGeophysical Journal International, 30
A. Şengör, Si̇lva Büyükaşikoğlu, N. Canitez (1983)
Neotectonics of the Pontides: implications for ‘incompatible’ structures along the North Anatolian faultJournal of Structural Geology, 5
U. Kuran, A. Yalciner (1993)
Crack Propagations, Earthquakes and Tsunamis in the Vicinity of Anatolia
[Black Sea is one of the biggest inland seas in the world covering an area of 461.000 km² where six countries share a common coastline. Turkish portion of the Black Sea coastline has a length of 1650 km along with 15 cities where 9 million people live. The region is the main fishery resource of Turkey while hosting country’s major ports, industrial facilities, specific regional agricultural products (tea, tobacco and nuts), offshore oil and gas production barges and a number of planned nuclear power plants. The coastline was prone to several big earthquakes, but went through three major tsunami events (Amasya 1598; Fatsa 1939; and Amasra 1968) in the past. Therefore the upcoming tsunami event in the future will be a major threat to the people of the region as well as economy of the country. In this study, a mixed discontinuous/continuous Galerkin finite element method is applied to solve the shallow water equations describing the long wave dynamics and representing a potential hazard modelling in the Black Sea. Discontinuous piecewise linear functions for velocity and continuous piecewise quadratic functions for sea level will be both utilized while the splitting method will be used with respect to time. Grid generator for Galerkin finite element method is based on unstructured triangular cells of variable size. The results of the simulation of the Black Sea level dynamics after initial shock suggest rather narrow alert/response time window of opportunity for the coastline of Turkey.]
Published: Jun 11, 2012
Keywords: Tsunami; Potential hazard; Modelling; Black Sea; Turkey
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