An application of the time- and magnitude-predictable model to long-term earthquake prediction in eastern Anatolia
In order to estimate the recurrence intervals for large earthquakes occurring in eastern Anatolia, this region enclosed within the coordinates of 36^sup ^-42^sup ^N, 35^sup ^-45^sup ^E has been separated into nine seismogenic sources on the basis of certain seismological and geomorphological criteri...
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Published in | Journal of seismology Vol. 9; no. 3; pp. 367 - 379 |
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Main Author | |
Format | Journal Article |
Language | English |
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Dordrecht
Springer
01.07.2005
Springer Nature B.V |
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Abstract | In order to estimate the recurrence intervals for large earthquakes occurring in eastern Anatolia, this region enclosed within the coordinates of 36^sup ^-42^sup ^N, 35^sup ^-45^sup ^E has been separated into nine seismogenic sources on the basis of certain seismological and geomorphological criteria, and a regional time- and magnitude-predictable model has been applied for these sources. This model implies that the magnitude of the preceding main shock which is the largest earthquake during a seismic excitation in a seismogenic source governs the time of occurrence and the magnitude of the expected main shock in this source. The data belonging to both the instrumental period (M^sub S^≥ 5.5) until 2003 and the historical period (I^sub 0^≥ 9.0 corresponding to M^sub S^≥ 7.0) before 1900 have been used in the analysis. The interevent time between successive main shocks with magnitude equal to or larger than a certain minimum magnitude threshold were considered in each of the nine source regions within the study area. These interevent times as well as the magnitudes of the main shocks have been used to determine the following relations: log T^sub t^ = 0.11M^sub min^ - 0.12M^sub p^ - 0.11 log M^sub 0^ + 2.51 M^sub f^ = 0.89M^sub min^ - 0.24M^sub p^ + 0.31 log M^sub 0^ - 4.99 where T^sub t^ is the interevent time measured in years, M^sub min^ is the surface wave magnitude of the smallest main shock considered, M^sub p^ is the magnitude of the preceding main shock, M^sub f^ is magnitude of the following main shock, and M^sub 0^ is the released seismic moment per year in each source. Multiple correlation coefficient and standard deviation have been computed as 0.50 and 0.28, respectively for the first relation. The corresponding values for the second relation are 0.64 and 0.32, respectively. It was found that the magnitude of the following main shock M^sub f^ does not depend on the preceding interevent time T^sub t^. This case is an interesting property for earthquake prediction since it provides the ability to predict the time of occurrence of the next strong earthquake. On the other hand, a strong negative dependence of M^sub f^ on M^sub p^ was found. This result indicates that a large main shock is followed by a smaller magnitude one and vice versa. On the basis of the first one of the relations above and taking into account the occurrence time and magnitude of the last main shock, the probabilities of occurrence P(Δ t) of main shocks in each seismogenic source of the east Anatolia during the next 10, 20, 30, 40 and 50 years for earthquakes with magnitudes equal 6.0 and 7.0 were determined. The second of these relations has been used to estimate the magnitude of the expected main shock. According to the time- and magnitude-predictable model, it is expected that a strong and a large earthquake can occur in seismogenic Source 2 (Erzincan) with the highest probabilities of P^sub 10^ = 66% (M^sub f^ = 6.9 and T^sub t^ = 12 years) and P^sub 10^ = 44% (M^sub f^ = 7.3 and T^sub t^ = 24 years) during the future decade, respectively.[PUBLICATION ABSTRACT] |
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AbstractList | In order to estimate the recurrence intervals for large earthquakes occurring in eastern Anatolia, this region enclosed within the coordinates of 36^sup ^-42^sup ^N, 35^sup ^-45^sup ^E has been separated into nine seismogenic sources on the basis of certain seismological and geomorphological criteria, and a regional time- and magnitude-predictable model has been applied for these sources. This model implies that the magnitude of the preceding main shock which is the largest earthquake during a seismic excitation in a seismogenic source governs the time of occurrence and the magnitude of the expected main shock in this source. The data belonging to both the instrumental period (M^sub S^≥ 5.5) until 2003 and the historical period (I^sub 0^≥ 9.0 corresponding to M^sub S^≥ 7.0) before 1900 have been used in the analysis. The interevent time between successive main shocks with magnitude equal to or larger than a certain minimum magnitude threshold were considered in each of the nine source regions within the study area. These interevent times as well as the magnitudes of the main shocks have been used to determine the following relations: log T^sub t^ = 0.11M^sub min^ - 0.12M^sub p^ - 0.11 log M^sub 0^ + 2.51 M^sub f^ = 0.89M^sub min^ - 0.24M^sub p^ + 0.31 log M^sub 0^ - 4.99 where T^sub t^ is the interevent time measured in years, M^sub min^ is the surface wave magnitude of the smallest main shock considered, M^sub p^ is the magnitude of the preceding main shock, M^sub f^ is magnitude of the following main shock, and M^sub 0^ is the released seismic moment per year in each source. Multiple correlation coefficient and standard deviation have been computed as 0.50 and 0.28, respectively for the first relation. The corresponding values for the second relation are 0.64 and 0.32, respectively. It was found that the magnitude of the following main shock M^sub f^ does not depend on the preceding interevent time T^sub t^. This case is an interesting property for earthquake prediction since it provides the ability to predict the time of occurrence of the next strong earthquake. On the other hand, a strong negative dependence of M^sub f^ on M^sub p^ was found. This result indicates that a large main shock is followed by a smaller magnitude one and vice versa. On the basis of the first one of the relations above and taking into account the occurrence time and magnitude of the last main shock, the probabilities of occurrence P(Δ t) of main shocks in each seismogenic source of the east Anatolia during the next 10, 20, 30, 40 and 50 years for earthquakes with magnitudes equal 6.0 and 7.0 were determined. The second of these relations has been used to estimate the magnitude of the expected main shock. According to the time- and magnitude-predictable model, it is expected that a strong and a large earthquake can occur in seismogenic Source 2 (Erzincan) with the highest probabilities of P^sub 10^ = 66% (M^sub f^ = 6.9 and T^sub t^ = 12 years) and P^sub 10^ = 44% (M^sub f^ = 7.3 and T^sub t^ = 24 years) during the future decade, respectively.[PUBLICATION ABSTRACT] In order to estimate the recurrence intervals for large earthquakes occurring in eastern Anatolia, this region enclosed within the coordinates of 36DG-42DGN, 35DG-45DGE has been separated into nine seismogenic sources on the basis of certain seismological and geomorphological criteria, and a regional time- and magnitude-predictable model has been applied for these sources. This model implies that the magnitude of the preceding main shock which is the largest earthquake during a seismic excitation in a seismogenic source governs the time of occurrence and the magnitude of the expected main shock in this source. The data belonging to both the instrumental period (Ms > 5.5) until 2003 and the historical period (I0 > 9.0 corresponding to Ms > 7.0) before 1900 have been used in the analysis. The interevent time between successive main shocks with magnitude equal to or larger than a certain minimum magnitude threshold were considered in each of the nine source regions within the study area. |
Author | SAYIL, Nilgün |
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Cites_doi | 10.1111/j.1467-7717.1981.tb01108.x 10.1111/j.1365-246X.1994.tb02136.x 10.1029/GL007i004p00279 10.1785/BSSA0740051767 10.1016/0040-1951(76)90159-1 10.1007/BF00876578 10.1785/BSSA0660030843 10.1111/j.1365-246X.1972.tb02351.x 10.1029/JB082i020p02981 10.1785/BSSA0340040185 10.3133/ofr7667 10.1029/GL006i009p00681 10.1126/science.288.5466.661 10.1111/j.1365-246X.1988.tb01387.x 10.1111/j.1365-246X.1997.tb05321.x 10.1186/BF03351630 10.1785/BSSA0690010115 10.1007/BF00945167 10.1016/0040-1951(90)90155-2 10.1029/GL004i002p00091 10.1038/332319a0 10.1016/S0040-1951(96)00252-1 10.1029/ME004p0297 |
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Keywords | earthquake prediction models Anatolia time- and magnitude-predictable model probability recurrence time coordinates mainshocks earthquakes surface waves Asia prediction magnitude seismic moment correlation coefficient standard deviation seismicity |
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References | B. Gutenberg (37_CR9) 1944; 34 37_CR19 N.N. Ambraseys (37_CR3) 1981; 5 37_CR18 B.C. Papazachos (37_CR28) 1993; 140 H. Kanamori (37_CR12) 1977; 82 J.F. Dewey (37_CR6) 1976; 66 H.K. Acharya (37_CR1) 1979; 6 İ. Osmansahin (37_CR22) 1986; 52 B.C. Papazachos (37_CR26) 1989; 79 T. Parsons (37_CR33) 2000; 288 L.R. Sykes (37_CR38) 1981; 4 G.F. Karakaisis (37_CR15) 2000; 52 B.C. Papazachos (37_CR29) 1994a; 84 B.C. Papazachos (37_CR31) 1997a; 149 P. Molnar (37_CR21) 1979; 69 37_CR30 D. McKenzie (37_CR20) 1972; 30 37_CR34 B.C. Papazachos (37_CR27) 1990; 178 37_CR10 D.G. Panagiotopoulos (37_CR24) 1995; 85 G. Ekström (37_CR8) 1988; 332 37_CR37 J. Jackson (37_CR11) 1988; 93 37_CR13 37_CR35 C.G. Bufe (37_CR5) 1977; 4 R.S. Stein (37_CR39) 1997; 128 K. Shimazaki (37_CR36) 1980; 7 E. Ayhan (37_CR4) 1987 37_CR2 B.C. Papazachos (37_CR32) 1997b; 271 37_CR40 Ö. Kenar (37_CR17) 1996; 30 37_CR7 G.F. Karakaisis (37_CR14) 1994a; 116 37_CR23 S.G. Wesnousky (37_CR41) 1984; 74 V. Karnik (37_CR16) 1968 37_CR25 |
References_xml | – ident: 37_CR18 – volume: 79 start-page: 77 year: 1989 ident: 37_CR26 publication-title: Bull. Seism. Soc. Am. contributor: fullname: B.C. Papazachos – ident: 37_CR37 – volume: 5 start-page: 355 year: 1981 ident: 37_CR3 publication-title: Disaster doi: 10.1111/j.1467-7717.1981.tb01108.x contributor: fullname: N.N. Ambraseys – volume: 116 start-page: 198 year: 1994a ident: 37_CR14 publication-title: Geophys. J. Int. doi: 10.1111/j.1365-246X.1994.tb02136.x contributor: fullname: G.F. Karakaisis – ident: 37_CR35 – volume: 7 start-page: 279 year: 1980 ident: 37_CR36 publication-title: Geophys. Res. Letters doi: 10.1029/GL007i004p00279 contributor: fullname: K. Shimazaki – volume: 74 start-page: 687 year: 1984 ident: 37_CR41 publication-title: Bull. Seism. Soc. Am. doi: 10.1785/BSSA0740051767 contributor: fullname: S.G. Wesnousky – ident: 37_CR10 – ident: 37_CR30 – ident: 37_CR2 doi: 10.1016/0040-1951(76)90159-1 – volume: 140 start-page: 593 year: 1993 ident: 37_CR28 publication-title: Pure Appl. Geophys. doi: 10.1007/BF00876578 contributor: fullname: B.C. Papazachos – volume: 66 start-page: 843 year: 1976 ident: 37_CR6 publication-title: Bull. Seism. Soc. Am. doi: 10.1785/BSSA0660030843 contributor: fullname: J.F. Dewey – volume: 30 start-page: 109 year: 1972 ident: 37_CR20 publication-title: Geophys. J. R. Astr. Soc. doi: 10.1111/j.1365-246X.1972.tb02351.x contributor: fullname: D. McKenzie – volume: 82 start-page: 2981 year: 1977 ident: 37_CR12 publication-title: J. Geophys. Res. doi: 10.1029/JB082i020p02981 contributor: fullname: H. Kanamori – ident: 37_CR7 – volume-title: Seismicity of the European Area year: 1968 ident: 37_CR16 contributor: fullname: V. Karnik – volume: 34 start-page: 185 year: 1944 ident: 37_CR9 publication-title: Bull. Seism. Soc. Am. doi: 10.1785/BSSA0340040185 contributor: fullname: B. Gutenberg – ident: 37_CR40 – volume: 30 start-page: 59 year: 1996 ident: 37_CR17 publication-title: Bull. IISEE contributor: fullname: Ö. Kenar – ident: 37_CR19 doi: 10.3133/ofr7667 – volume: 6 start-page: 681 year: 1979 ident: 37_CR1 publication-title: Geophys. Res. Letters doi: 10.1029/GL006i009p00681 contributor: fullname: H.K. Acharya – volume: 288 start-page: 661 year: 2000 ident: 37_CR33 publication-title: Science doi: 10.1126/science.288.5466.661 contributor: fullname: T. Parsons – volume: 93 start-page: 45 year: 1988 ident: 37_CR11 publication-title: Geophys. J. doi: 10.1111/j.1365-246X.1988.tb01387.x contributor: fullname: J. Jackson – volume: 85 start-page: 1190 year: 1995 ident: 37_CR24 publication-title: Bull. Seism. Soc. Am. contributor: fullname: D.G. Panagiotopoulos – volume: 128 start-page: 594 year: 1997 ident: 37_CR39 publication-title: Geophys. J. Intern. doi: 10.1111/j.1365-246X.1997.tb05321.x contributor: fullname: R.S. Stein – ident: 37_CR13 – ident: 37_CR34 – volume: 84 start-page: 426 year: 1994a ident: 37_CR29 publication-title: Bull. Seism. Soc. Am. contributor: fullname: B.C. Papazachos – volume: 52 start-page: 221 year: 2000 ident: 37_CR15 publication-title: Earth Planets Space doi: 10.1186/BF03351630 contributor: fullname: G.F. Karakaisis – volume: 69 start-page: 115 year: 1979 ident: 37_CR21 publication-title: Bull. Seism. Soc. Am. doi: 10.1785/BSSA0690010115 contributor: fullname: P. Molnar – volume: 52 start-page: 5 year: 1986 ident: 37_CR22 publication-title: Bull. Earthquake Res Ints. of Türkiye contributor: fullname: İ. Osmansahin – volume: 149 start-page: 173 year: 1997a ident: 37_CR31 publication-title: Pure Appl. Geophys. doi: 10.1007/BF00945167 contributor: fullname: B.C. Papazachos – volume-title: An Earthquake Catalogue of Turkey and Surrounding Area (1881–1980) year: 1987 ident: 37_CR4 contributor: fullname: E. Ayhan – volume: 178 start-page: 287 year: 1990 ident: 37_CR27 publication-title: Tectonophys doi: 10.1016/0040-1951(90)90155-2 contributor: fullname: B.C. Papazachos – volume: 4 start-page: 91 year: 1977 ident: 37_CR5 publication-title: Geophys. Res. Letters doi: 10.1029/GL004i002p00091 contributor: fullname: C.G. Bufe – volume: 332 start-page: 319 year: 1988 ident: 37_CR8 publication-title: Nature doi: 10.1038/332319a0 contributor: fullname: G. Ekström – volume: 271 start-page: 295 year: 1997b ident: 37_CR32 publication-title: Tectonophys doi: 10.1016/S0040-1951(96)00252-1 contributor: fullname: B.C. Papazachos – ident: 37_CR25 – ident: 37_CR23 – volume: 4 start-page: 297 year: 1981 ident: 37_CR38 publication-title: Maurice Ewing Series doi: 10.1029/ME004p0297 contributor: fullname: L.R. Sykes |
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Snippet | In order to estimate the recurrence intervals for large earthquakes occurring in eastern Anatolia, this region enclosed within the coordinates of 36^sup... In order to estimate the recurrence intervals for large earthquakes occurring in eastern Anatolia, this region enclosed within the coordinates of 36DG-42DGN,... |
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SubjectTerms | Correlation coefficient Earth sciences Earth, ocean, space Earthquake prediction Earthquakes Earthquakes, seismology Engineering and environment geology. Geothermics Exact sciences and technology Internal geophysics Natural hazards: prediction, damages, etc Seismic activity Seismology Standard deviation |
Title | An application of the time- and magnitude-predictable model to long-term earthquake prediction in eastern Anatolia |
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