Abstract
The Mw 7.4 Izmit earthquake of 17 August 1999 struck a part ofthe North Anatolian fault in the area of Izmit Bay (NW Turkey). Historicalinformation shows that the fault which moved during the generation of thisearthquake consists of two fault segments moved during the generation oflarge (M ∼ 7) earthquakes in 1719 and 1754, respectively. Since then onlythe central part (between Izmit and Lake Sapanca) of this fault ruptured bythe generation of a smaller shock (M = 6.6) in 1878.The spatial stress variations based on the calculation of changes in theCoulomb Failure Function (ΔCFF) associated with this earthquake aresupported by the distribution of strong aftershock foci. Large positive valuesof ΔCFF to the east and west of the mainshock epicenter are inagreement with the notion that secondary faults were triggered there by thegeneration of the main event. Large positive values of ΔCFF are alsoobserved in the adjacent western fault segment where the 1766 event wasgenerated, evidencing the occurrence of the next strong earthquake in thissegment.
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References
Allen, C.R., 1969, Active faulting in northern Turkey, Contrib. 1577, Div. Geol. Sci., Calif. Inst. Technol., 32 pp.
Ambraseys, N.N. and Zatopek, A., 1969, The Mudurnu valley, west Anatolia, Turkey, earthquake of 22 July 1967. Bull. Seismol. Soc. Am. 59, 521–589.
Ambraseys, N.N. and Finkel, C.F., 1995, The Seismicity of Turkey and Adjacent Areas: A Historical Review, 1500–1800, Istanbul: Muhittin Salih EREN, 1995.
Ambraseys, N.N. and Jackson, J.A., 2000, Seismicity of the Sea of Marmara (Turkey) since 1500. Geophys. J. Int. 141, F1–F6.
Baba, A.B., Papadimitriou, E.E., Papazachos, B.C., Papaioannou, Ch.A. and Karakostas, B.G., 2000, A unified local magnitude scale for earthquakes of south Balkan area, Pure Appl. Geophys. 157, 765–783.
Barka, A.A., 1999, 17 August 1999 earthquake. Science 258, 1858–1859.
Barka, A. and Kadinsky-Cade, K., 1988, Strike-slip fault geometry in Turkey and its influence on earthquake activity. Tectonics 7, 663–684.
Das, S. and Scholz, C., 1982, Off-fault aftershock clusters caused by shear stress increase— Bull. Seismol. Soc. Am. 72, 1669–1675.
Deng, J. and Sykes, L.R., 1997a, Evolution of the stress field in southern California and triggering of moderate-size earthquakes: A 200-year perspective, J. Geophys. Res. 102, 9859–9886.
Deng, J. and Sykes, L.R., 1997b, Stress evolution in southern California and triggering of moderate-, small-, and micro-size earthquakes, J. Geophys. Res. 102, 24,411–24,435.
Dewey, J.W., 1976, Seismicity of northern Anatolia, Bull. Seismol. Soc. Am. 66, 843–868.
Erikson, L., 1986, User'smanual for DIS3D: A three-dimensional dislocation program with applications to faulting in the Earth, Masters Thesis, Stanford Univ., Stanford, Calif., 167 pp.
Georgiadis, S.A., 1904, About Earthquakes and Antiseismic Constructions, Publ. S. Kousoulinou, Athens, 306 pp (in Greek).
Guidoboni, E., Comastri, A. and Traina, G., 1994, Catalogue of Ancient Earthquakes in theMediterranean Area up to 10th Century, SGA Storia Geofisica Ambiente, Bologna, 504 pp.
Hardebeck, J.L., Nazareth, J.J. and Hauksson, E., 1998, The static stress change triggering model: Constraints from two southern California aftershock sequences J. Geophys. Res. 103, 24,427–24,437.
Harris, R.A. and Simpson, R.W., 1993. In the shadow of 1857, an evaluation of the stress changes generated by the M8 Ft. Tejon, California, earthquake (abstract), Eos Trans. AGU, 74(43), Fall Meet. Suppl., 427.
Harris, R.A. and Simpson, R.W., 1996. In the shadow of the 1857 – The effect of the great Ft. Tejon earthquake on the subsequent earthquakes in southern California, Geophys. Res. Lett. 23, 229–232.
Hubert-Ferrari, A., Barka, A., Jacques, E., Nalbant, S.S., Meyer, B., Armijo, R., Tapponnier, P. and King, G.C.P., 2000, Seismic hazard in the Marmara sea region following the 17 August 1999 Izmit earthquake, Nature 404, 269–273.
Jackson, J. and McKenzie, D.P., 1988, The relationship between plate motions and seismic moment tensors, and the rates of active deformation in the Mediterranean and Middle East, Geophys. J. Int. 93, 45–73.
Karakaisis, G.F., Karakostas, B.G., Papadimitriou, E.E., Scordilis, E.M. and Papazachos, B.C., 1985, Seismic sequences in Greece interpreted in terms of barrier model, Nature 315, 212–214.
Karnik, V., 1971, Seismicity of the European Area, Part II, 1801–1900, D. Reidel Publ. Comp. Dordrecht, Netherlands, 218 pp.
Kasahara, K., 1981, Earthquake Mechanics, Cambridge Univ. Press, Cambridge.
King, G.C.P., Stein, R.S. and Lin, J., 1994a, Static stress changes and the triggering of earthquakes, Bull. Seism. Soc. Am. 84, 935–953.
King, G., Oppenheimer, D. and Amelung, F., 1994b, Block versus continuum deformation in the western United States, Earth Planet. Sci. Lett. 128, 55–64.
KOERI, Seismological Obs., Turkiye.
Margaris, B.N. and Papazachos, C.B., 1999, Moment magnitude relations based on strong motion records in Greece, Bull. Seismol. Soc. Am. 89, 442–455.
Mogi, K., 1985, Earthquake Prediction, Academic Press, Tokyo.
Nalbant, S.S., Hubert, A. and King, C.P., 1998, Stress coupling between earthquakes in northwest Turkey and the northern Aegean, J. Geophys. Res. 103, 24,469–24,486.
Okada, Y., 1992, Internal deformation due to shear and tensile faults in a half-space, Bul. Seismol. Soc. Am. 82, 1018–1040.
Papazachos, B.C., 1989, Measures of Earthquake Size in Greece and Surrounding Areas, Proc. Of the 1st Scient. Conf. Of Geophysics, Geophys. Soc. Of Greece, April 19–21, 1989, Athens, pp. 438–447.
Papazachos, B.C. and Papazachou, C.B., 1997, The earthquakes of Greece. Ziti Publ., Thessaloniki, 304 pp.
Papazachos, B.C., Kiratzi, A.A. and Karakostas, V.G., 1997a, Toward a homogeneous moment magnitude determination in Greece and surrounding area, Bull. Seism. Soc. Am. 87, 474–483.
Papazachos, B.C., Papaioannou, Ch.A., Papazachos, C.B. and Savvaidis, A.S., 1997b, Atlas of isoseismal maps for strong earthquakes in Greece and surrounding area (426BC–1995), Publ. Geophys. Lab., Univ. Thessaloniki 4, 192 pp.
Papazachos, B.C., Karakaisis, G.F., Papadimitriou, E.E. and Papaioannou, Ch.A., 1997c, The regional time and magnitude predictable model and its application to the Alpine-Himalayan belt, Tectnophysics 271, 295–323.
Papazachos, C.B., 1992, Anisotropic radiation modeling of macroseismic intensities for estimation of the attenuation structure of the upper crust in Greece, Pure appl. Geophys. 138, 445–469.
Papazachos, C.B. and Papaioannou, Ch.A., 1997, The macroseismic field in the Balkan area, J. Seismology 1, 181–201.
Parsons, T., Toda, S., Stein, R.S., Barka, A. and Dieterich, J.H., 2000, Heightened odds of large earthquakes near Istanbul: An interaction-based probability calculation, Science 288, 661–665.
Reasenberg, P.A. and Simpson, R.W., 1992, Response of regional seismicity to the static stress change produced by the Loma Prieta earthquake, Science 255, 1687–1690.
Richter, C.F., 1958, Elementary Seismology, San Francisco: W.H. Freeman & Co.
Scholz, C., 1990, The Mechanics of Earthquakes and Faulting, Cambridge University Press, Cambridge, 439 pp.
Stein, R.S., Barka, A.A. and Dieterich, J.H., 1997, Progressive failure of the North Anatolian fault since 1939 by earthquake stress triggering, Geophys. J. Int. 128, 594–604.
Toksoz, M.N., Shakal, A.F. and Michael, A.J., 1979, Space-time migration of earthquakes along the North Anatolian Fault Zone and seismic gaps, Pure Appl. Geophys. 117, 1258–1270.
Wells, D.L. and Coppersmith, K.J., 1994, New empirical relationships among magnitude, rupture length, rupture width, rupture are, and surface displacement, Bull. Seism. Soc. Am. 84, 974–1002.
Wessel, P. and Smith, W.H.F., 1991, Free software helps map and display data, Eos, Trans. AGU 72, 441, 445–446.
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Papadimitriou, E., Karakostas, V. & Papazachos, B. Rupture zones in the area of the 17.08.99 Izmit (NW Turkey) large earthquake (Mw 7.4) and stress changes caused by its generation. Journal of Seismology 5, 269–276 (2001). https://doi.org/10.1023/A:1011463420557
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DOI: https://doi.org/10.1023/A:1011463420557