Investigation of the effect areas and occurred deformation due to major earthquakes is a significant finding for geosciences. Major earthquakes create displacement and deformation in great areas with the effect of co-seismic and postseismic movements. In this study, the earthquake, which was occurred at 24th May 2014 with Ml=6.5 offshore of Gökçeada (Imbros) in Aegean Sea and was felt in Marmara and Aegean regions, was handled and the effects of the earthquakes were examined. Marmara and Aegean regions were selected as the study area and 13 days GPS data, which included pre-seismic, coseismic and post-seismic effects, were processed of 14 continuous GNSS stations of CORS-TR (TUSAGA-Aktif) and the movements of these stations were figured out by examining the time-series. Consequently, it has been determined that this earthquake has affected all of the 14 stations and caused the deformation
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viscoelastic postseismic
deformation due to large
earthquakes in East Anatolia,
Turkey, Journal of Geodynamics,
Cilt. 94–95, s. 25-33.
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Temporal evolution of continental
lithospheric strength in actively
deforming regions, GSA Today,
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[3] Pollitz, F. F., Wicks, C., Thatcher,
W. 2001. Mantle flow beneath a
continental strike-slip fault:
Postseismic deformation after the
1999 Hector Mine earthquake,
Science, Cilt. 293(5536), s. 1814-
1818.
[4] Kenner, S. J., Segall, P., 2003.
Lower crustal structure in
northern California: Implications
from strain rate variations
following the 1906 San Francisco
earthquake, Journal of
Geophysical Research: Solid Earth,
108(B1).
[5] Freed, A. M., Burgmann, R., 2004.
Evidence of power-law flow in the
Mojave desert mantle, Nature, Cilt.
430(6999), s. 548.
[6] Freed, A. M., Lin, J. 2001. Delayed
triggering of the 1999 Hector Mine
earthquake by viscoelastic stress
transfer, Nature, Cilt. 411(6834), s.
180.
[7] Rydelek, P. A., Sacks, I. S., 2001.
Migration of large earthquakes
along the San Jacinto fault; stress
diffusion from the 1857 Fort
Tejon earthquake, Geophysical
research letters, Cilt. 28(16), s.
3079-3082.
[8] Chery, J., Carretier, S., Ritz, J.F.,
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explains time clustering of large
earthquakes in Mongolia, Earth
and Planetary Sciences Letters, Cilt.
194, s. 277–286.
[9] Casarotti, E., Piersanti, A., Lucente,
F.P., Boschi, E. 2001. Global
postseismic stress diffusion and
fault interaction at long distances,
Earth and Planetary Sciences
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[10] Pollitz, F., Bürgmann, R.,
Romanowicz, B. 1998. Viscosity of
oceanic asthenosphere inferred
from remote triggering
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1245–1249.
[11] Nalbant, S.S., McCloskey, J. 2011.
Stress evolution before and after
the 2008 Wenchuan, China
earthquake, Earth and Planetary
Sciences Letters, Cilt. 307, s. 222–
232.
[12] Kahveci, M., Yıldız, F. 2009.
GPS/GNSS uydularla konum
belirleme sistemleri, uygulamateori,
4. baskı. Ankara, Nobel, 220s.
[13] Yu, S.B., Hsu, Y.J., Kuo, L.C., Chen,
H.,Y., Liu, C. C. 2003. GPS
measurement of postseismic
deformation following the 1999
Chi-Chi, Taiwan, earthquake,
Journal of Geophysical Research,
Cilt. 108, s. 2520.
[14] Serpelloni, E., Vannucci, G.,
Anderlini, L., Bennett, R. A. 2016.
Kinematics, seismotectonics and
seismic potential of the Eastern
sector of the European Alps from
GPS and seismic deformation data,
Tectonophysics, Cilt. 688, s. 157-
181.
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Present-day dynamics of the
Aegean region: A model analysis of
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879– 895.
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eastern Mediterranean kinematics,
Geophysical Research Letters, Cilt.
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Subduction and slab detachment in
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1917.
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Babbucci, D. 2001. Short and long
term deformation patterns in the
Aegean-Anatolian system: Insights
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Geophysical Research Letters, Cilt.
28, s. 2325– 2328.
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The block-like behavior of Anatolia
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geodetic strain rates, Geophysical
Research Letters, Cilt. 29(20), s.
1978. doi:10.1029/2002GL015995
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R.E. 2002. Viscoelastic deformation
from North Anatolian Fault Zone
earthquakes and the eastern
Mediterranean GPS velocity field,
Geophysical Research Letters, Cilt. 29(11), s. 1549.
doi:10.1029/2002GL014889
[21] Provost, A.S., Chery, J., Hassani, R.
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the GPS velocity field along the
North Anatolian fault, Earth and
Planetary Science Letters, Cilt. 209,
s. 361– 377.
[22] Flerit, F., Armijo, R., King, G., Meyer,
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Geiger, A., Reilinger, R., Barka, A.,
Veis, G. 2000. GPS-derived strain
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the Eurasian, African, and Arabian
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23.353–23.370.
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Tealeb, A., Toksöz, M.N., Veis, G.
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Journal of Geophysical Research,
Cilt. 105(B3), s. 5695–5719.
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constraints on the active tectonic
deformation of the Aegean, Journal
of Geophysical Research, Cilt. 109,
B11406. doi:10.1029/
2003JB002830
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coupling on the Hellenic
subduction plate interface, Earth
and Planetary Science Letters, Cilt.
385, s. 122–129.
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A., Kahle, H.G. 2008. Crustal motion
and deformation in Greece from a
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449 (1–4), s. 17–40.
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Deformation of western Turkey
from a combination of permanent
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block-like behavior, Journal of
Geophysical Research, Cilt. 114, s.
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surrounding using repeated
GPS/GNSS observations:
Preliminary Results. 15th General
Assembly of Wegener, 14-17 Eylül,
İstanbul, 7
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M., Şalk, M., Gönenç, T., Ersay, E.,
Ergintav, S., Belgen, A. 2010b.
Evaluation of microgravity and
GPS/GNSS data together by the
network system and a case study in
İzmir (Western Turkey). 10th
International Multidisciplinary
Scientific Geoconference SGEM
2010, 20-16 Haziran, Albena,
Bulgaristan, 777-782.
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Sındırgı, P., Kaftan, I., Akdemir, Ö.
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mass changes in the south of Izmir
(Turkey) by monitoring
microgravity and GPS/GNSS
methods, Journal of Earth System
Science, Cilt. 124, No. 1, s. 137–148.
[34] Pamukçu, O., Gönenç, T., Çırmık,
Y.A., Kahveci, M. 2015b.
Investigation of the Sıgacık Bay’s
displacement characteristic by
using GPS and gravity data in
Western Anatolia, Journal of Asian
Earth Scince, Cilt. 99, s. 72–84.
[35] Çırmık, A. 2014. Determining the
deformations in Western Anatolia
with GPS and gravity
measurements. Doktora Tezi,
Dokuz Eylül Üniversitesi, Fen
Bilmleri Enstitüsü, İzmir.
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the Menderes Massif (Western
Anatolia, Turkey), Journal of Asian
Earth Science, Cilt. 131, s. 109-122.
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24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ
Yıl 2018,
Cilt: 20 Sayı: 58, 230 - 244, 01.01.2018
Bir depremin etki alanının ve meydana getirdiği deformasyonların incelenmesi yerbilimleri açısından önemli bir bulgudur. Büyük depremler deprem anı ve deprem sonrasında büyük alanlarda yer değiştirme ve deformasyonlar meydana getirmektedir. Bu çalışmada, 24 Mayıs 2014 tarihinde Gökçeada açıkları Ege Denizi’nde Ml=6,5 büyüklüğünde meydana gelen deprem ele alınmış, Marmara ve Ege Bölgeleri’nde hissedilen bu depremin yer değiştirme etkileri irdelenmiştir. Çalışma alanı olan Marmara ve Ege Bölgeleri’nde kurulu 14 adet TUSAGA-Aktif sistemine ait sürekli GNSS istasyonlarının deprem öncesi, deprem anı ve deprem sonrasını içeren 13 günlük GPS verisi çözümlenerek, bu istasyonların bu depreme bağlı olarak nasıl hareket ettiği, bu istasyonların zaman serilerinin incelenmesiyle ortaya konmuştur. Sonuç olarak, bu depremin 14 adet istasyonunun tümünü etkilediği ve deformasyonlara neden olduğu görülmüştür
[1] Sunbul, F., Nalbant, S.S., Simão
N.M., Steacy, S. 2016. Investigating
viscoelastic postseismic
deformation due to large
earthquakes in East Anatolia,
Turkey, Journal of Geodynamics,
Cilt. 94–95, s. 25-33.
[2] Thatcher, W., Pollitz, F.F. 2008.
Temporal evolution of continental
lithospheric strength in actively
deforming regions, GSA Today,
Cilt. 18, s. 4–11.
[3] Pollitz, F. F., Wicks, C., Thatcher,
W. 2001. Mantle flow beneath a
continental strike-slip fault:
Postseismic deformation after the
1999 Hector Mine earthquake,
Science, Cilt. 293(5536), s. 1814-
1818.
[4] Kenner, S. J., Segall, P., 2003.
Lower crustal structure in
northern California: Implications
from strain rate variations
following the 1906 San Francisco
earthquake, Journal of
Geophysical Research: Solid Earth,
108(B1).
[5] Freed, A. M., Burgmann, R., 2004.
Evidence of power-law flow in the
Mojave desert mantle, Nature, Cilt.
430(6999), s. 548.
[6] Freed, A. M., Lin, J. 2001. Delayed
triggering of the 1999 Hector Mine
earthquake by viscoelastic stress
transfer, Nature, Cilt. 411(6834), s.
180.
[7] Rydelek, P. A., Sacks, I. S., 2001.
Migration of large earthquakes
along the San Jacinto fault; stress
diffusion from the 1857 Fort
Tejon earthquake, Geophysical
research letters, Cilt. 28(16), s.
3079-3082.
[8] Chery, J., Carretier, S., Ritz, J.F.,
2001. Postseismic stress transfer
explains time clustering of large
earthquakes in Mongolia, Earth
and Planetary Sciences Letters, Cilt.
194, s. 277–286.
[9] Casarotti, E., Piersanti, A., Lucente,
F.P., Boschi, E. 2001. Global
postseismic stress diffusion and
fault interaction at long distances,
Earth and Planetary Sciences
Letters, Cilt. 191, s. 75–84.
[10] Pollitz, F., Bürgmann, R.,
Romanowicz, B. 1998. Viscosity of
oceanic asthenosphere inferred
from remote triggering
earthquakes, Science, Cilt. 280, s..
1245–1249.
[11] Nalbant, S.S., McCloskey, J. 2011.
Stress evolution before and after
the 2008 Wenchuan, China
earthquake, Earth and Planetary
Sciences Letters, Cilt. 307, s. 222–
232.
[12] Kahveci, M., Yıldız, F. 2009.
GPS/GNSS uydularla konum
belirleme sistemleri, uygulamateori,
4. baskı. Ankara, Nobel, 220s.
[13] Yu, S.B., Hsu, Y.J., Kuo, L.C., Chen,
H.,Y., Liu, C. C. 2003. GPS
measurement of postseismic
deformation following the 1999
Chi-Chi, Taiwan, earthquake,
Journal of Geophysical Research,
Cilt. 108, s. 2520.
[14] Serpelloni, E., Vannucci, G.,
Anderlini, L., Bennett, R. A. 2016.
Kinematics, seismotectonics and
seismic potential of the Eastern
sector of the European Alps from
GPS and seismic deformation data,
Tectonophysics, Cilt. 688, s. 157-
181.
[15] Meijer, P.T., Wortel, M.J.R 1997.
Present-day dynamics of the
Aegean region: A model analysis of
the horizontal pattern of stress and
deformation, Tectonics, Cilt. 16, s.
879– 895.
[16] Lundgren, P., Giardini, D., Russo, R.
1998. A geodynamic framework for
eastern Mediterranean kinematics,
Geophysical Research Letters, Cilt.
25, s. 4007– 4010.
[17] Wortel, M.J.R., Spakman, W. 2000.
Subduction and slab detachment in
the Mediterranean-Carpathian
region, Science, Cilt. 290, s. 1910–
1917.
[18] Mantovani, E., Viti, M., Cenni, N.,
Babbucci, D. 2001. Short and long
term deformation patterns in the
Aegean-Anatolian system: Insights
from space-geodetic data (GPS),
Geophysical Research Letters, Cilt.
28, s. 2325– 2328.
[19] Jimenez-Munt, I., Sabadini, R. 2002.
The block-like behavior of Anatolia
envisaged in the modeled and
geodetic strain rates, Geophysical
Research Letters, Cilt. 29(20), s.
1978. doi:10.1029/2002GL015995
[20] Hearn, E.H., Hager, B.H., Reilinger,
R.E. 2002. Viscoelastic deformation
from North Anatolian Fault Zone
earthquakes and the eastern
Mediterranean GPS velocity field,
Geophysical Research Letters, Cilt. 29(11), s. 1549.
doi:10.1029/2002GL014889
[21] Provost, A.S., Chery, J., Hassani, R.
2003. 3D mechanical modeling of
the GPS velocity field along the
North Anatolian fault, Earth and
Planetary Science Letters, Cilt. 209,
s. 361– 377.
[22] Flerit, F., Armijo, R., King, G., Meyer,
B., Barka, A. 2003. Slip-partitioning
in the Sea of Marmara pull-apart
determined from GPS velocity
vectors, Geophysical Journal
International, Cit. 154, s. 1–7.
[23] Reilinger, R., McClusky, S.,
Paradissis, D., Ergintav, S., Vernant,
P. 2010. Geodetic constraints on
the tectonic evolution of the
Aegean region and strain
accumulation along the Hellenic
subduction zone, Tectonophysics,
Cilt. 488, s. 22–30.
[24] Kahle, H.G., Cocard, M., Peter, Y.,
Geiger, A., Reilinger, R., Barka, A.,
Veis, G. 2000. GPS-derived strain
field within the boundary zone of
the Eurasian, African, and Arabian
plates, Journal of Geophysical
Research, Cilt. 105 (B10), s.
23.353–23.370.
[25] McClusky, S., Balassanian, S., Barka,
A., Demir, C., Ergintav, S., Georgiev,
I., Gurkan, O., Hamburger, M.,
Hurst, K., Kahle, H., Kastens, K.,
Kekelidze, G., King, R., Kotzev, V.,
Lenk, O., Mahmoud, S., Mishin, A.,
Nadariya, M., Ouzounis, A.,
Paradissis, D., Peter, Y., Prilepin, M.,
Reilinger, R., Sanli, I., Seeger, H.,
Tealeb, A., Toksöz, M.N., Veis, G.
2000. Global Positioning System
constraints on plate kinematics
and dynamics in the eastern
Mediterranean and Caucasus,
Journal of Geophysical Research,
Cilt. 105(B3), s. 5695–5719.
[26] Nyst, M., Thatcher, W. 2004. New
constraints on the active tectonic
deformation of the Aegean, Journal
of Geophysical Research, Cilt. 109,
B11406. doi:10.1029/
2003JB002830
[27] Vernant, P., Reilinger, R., McClusky,
S. 2014. Geodetic evidence for low
coupling on the Hellenic
subduction plate interface, Earth
and Planetary Science Letters, Cilt.
385, s. 122–129.
[28] Hollenstein, C., Müller, M.D., Geiger,
A., Kahle, H.G. 2008. Crustal motion
and deformation in Greece from a
decade of GPS measurements,
1993–2003, Tectonophysics, Cilt.
449 (1–4), s. 17–40.
[29] Aktug, B., Nocquet, J.M., Cingoz, A.,
Parsons, B., Erkan, Y., England, P.,
Lenk, O., Gurda, M.A., Kilicoglu, A.,
Akdeniz, H., Tekgul, A. 2009.
Deformation of western Turkey
from a combination of permanent
and campaign GPS data: Limits to
block-like behavior, Journal of
Geophysical Research, Cilt. 114, s.
1–22.
[30] Floyd, M.A., Billiris, H., Paradissis,
D., Veis, G., Avallone, A., Briole, P.,
McClusky, S., Nocquet, J.M.,
Palamartchouk, K., Parsons, B.,
England, P.C. 2010. A new velocity
field for Greece: Implications for
the kinematics and dynamics of the
Aegean, Journal of Geophysical
Research, Cilt. 115, B10403.
[31] Pamukçu, O., Kahveci, M., Ersay,
E.Y., Yurdakul, A., Şalk, M., Sözbilir,
H. 2010a. Determination of the
kinematic structure of Izmir and
surrounding using repeated
GPS/GNSS observations:
Preliminary Results. 15th General
Assembly of Wegener, 14-17 Eylül,
İstanbul, 7
[32] Pamukçu, O., Yurdakul, A., Kahveci,
M., Şalk, M., Gönenç, T., Ersay, E.,
Ergintav, S., Belgen, A. 2010b.
Evaluation of microgravity and
GPS/GNSS data together by the
network system and a case study in
İzmir (Western Turkey). 10th
International Multidisciplinary
Scientific Geoconference SGEM
2010, 20-16 Haziran, Albena,
Bulgaristan, 777-782.
[33] Pamukçu, O., Gönenç, T., Çırmık, A.,
Sındırgı, P., Kaftan, I., Akdemir, Ö.
2015a. Investigation of vertical
mass changes in the south of Izmir
(Turkey) by monitoring
microgravity and GPS/GNSS
methods, Journal of Earth System
Science, Cilt. 124, No. 1, s. 137–148.
[34] Pamukçu, O., Gönenç, T., Çırmık,
Y.A., Kahveci, M. 2015b.
Investigation of the Sıgacık Bay’s
displacement characteristic by
using GPS and gravity data in
Western Anatolia, Journal of Asian
Earth Scince, Cilt. 99, s. 72–84.
[35] Çırmık, A. 2014. Determining the
deformations in Western Anatolia
with GPS and gravity
measurements. Doktora Tezi,
Dokuz Eylül Üniversitesi, Fen
Bilmleri Enstitüsü, İzmir.
[36] Çırmık, A., Pamukçu, O., Akçığ, Z.
2016a. Mass and stress changes in
the Menderes Massif (Western
Anatolia, Turkey), Journal of Asian
Earth Science, Cilt. 131, s. 109-122.
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Çırmık, A. (2018). 24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen Ve Mühendislik Dergisi, 20(58), 230-244.
AMA
Çırmık A. 24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ. DEUFMD. Ocak 2018;20(58):230-244.
Chicago
Çırmık, Ayça. “24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ”. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen Ve Mühendislik Dergisi 20, sy. 58 (Ocak 2018): 230-44.
EndNote
Çırmık A (01 Ocak 2018) 24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen ve Mühendislik Dergisi 20 58 230–244.
IEEE
A. Çırmık, “24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ”, DEUFMD, c. 20, sy. 58, ss. 230–244, 2018.
ISNAD
Çırmık, Ayça. “24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ”. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen ve Mühendislik Dergisi 20/58 (Ocak 2018), 230-244.
JAMA
Çırmık A. 24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ. DEUFMD. 2018;20:230–244.
MLA
Çırmık, Ayça. “24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ”. Dokuz Eylül Üniversitesi Mühendislik Fakültesi Fen Ve Mühendislik Dergisi, c. 20, sy. 58, 2018, ss. 230-44.
Vancouver
Çırmık A. 24 MAYIS 2014 GÖKÇEADA AÇIKLARI – EGE DENİZİ DEPREMİNİN (ML=6.5) DEPREM ANI VE SONRASI MEYDANA GETİRDİĞİ YER DEĞİŞTİRMELER VE DEFORMASYONLARIN İRDELENMESİ. DEUFMD. 2018;20(58):230-44.