Gas and seismicity within the Istanbul seismic gap

L. Géli; P. Henry; C. Grall; J. B. Tary; A. Lomax; E. Batsi; V. Riboulot; E. Cros; C. Gürbüz; S. E. Işlk; A. M.C. Sengör; X. Le Pichon; L. Ruffine; S. Dupré; Y. Thomas; D. Kalafat; G. Bayrakci; Q. Coutellier; T. Regnier; G. Westbrook; H. Saritas; G. Çifçi; M. N. Çaǧatay; M. S. Özeren; N. Görür; M. Tryon; M. Bohnhoff; L. Gasperini; F. Klingelhoefer; C. Scalabrin; J. M. Augustin; D. Embriaco; G. Marinaro; F. Frugoni; S. Monna; G. Etiope; P. Favali; A. Bécel

doi:10.1038/s41598-018-23536-7

Gas and seismicity within the Istanbul seismic gap

L. Géli^*, P. Henry, C. Grall, J. B. Tary, A. Lomax, E. Batsi, V. Riboulot, E. Cros, C. Gürbüz, S. E. Işlk, A. M.C. Sengör, X. Le Pichon, L. Ruffine, S. Dupré, Y. Thomas, D. Kalafat, G. Bayrakci, Q. Coutellier, T. Regnier, G. WestbrookH. Saritas, G. Çifçi, M. N. Çaǧatay, M. S. Özeren, N. Görür, M. Tryon, M. Bohnhoff, L. Gasperini, F. Klingelhoefer, C. Scalabrin, J. M. Augustin, D. Embriaco, G. Marinaro, F. Frugoni, S. Monna, G. Etiope, P. Favali, A. Bécel

^*Bu çalışma için yazışmadan sorumlu yazar

Avrasya Yer Bilimleri Enstitüsü

Araştırma sonucu: Dergiye katkı › Makale › bilirkişi

24 Atıf (Scopus)

Özet

Understanding micro-seismicity is a critical question for earthquake hazard assessment. Since the devastating earthquakes of Izmit and Duzce in 1999, the seismicity along the submerged section of North Anatolian Fault within the Sea of Marmara (comprising the "Istanbul seismic gap") has been extensively studied in order to infer its mechanical behaviour (creeping vs locked). So far, the seismicity has been interpreted only in terms of being tectonic-driven, although the Main Marmara Fault (MMF) is known to strike across multiple hydrocarbon gas sources. Here, we show that a large number of the aftershocks that followed the M 5.1 earthquake of July, 25^th 2011 in the western Sea of Marmara, occurred within a zone of gas overpressuring in the 1.5-5 km depth range, from where pressurized gas is expected to migrate along the MMF, up to the surface sediment layers. Hence, gas-related processes should also be considered for a complete interpretation of the micro-seismicity (~M < 3) within the Istanbul offshore domain.

Orijinal dil	İngilizce
Makale numarası	6819
Dergi	Scientific Reports
Hacim	8
Basın numarası	1
DOI'lar	https://doi.org/10.1038/s41598-018-23536-7
Yayın durumu	Yayınlandı - 1 Ara 2018

Bibliyografik not

Publisher Copyright:
© 2018 The Author(s).

BM SKH

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Belgeye Erişim

10.1038/s41598-018-23536-7

Diğer Dosyalar ve Linkler

Link to publication in Scopus

Alıntı Yap

Géli, L., Henry, P., Grall, C., Tary, J. B., Lomax, A., Batsi, E., Riboulot, V., Cros, E., Gürbüz, C., Işlk, S. E., Sengör, A. M. C., Le Pichon, X., Ruffine, L., Dupré, S., Thomas, Y., Kalafat, D., Bayrakci, G., Coutellier, Q., Regnier, T., ... Bécel, A. (2018). Gas and seismicity within the Istanbul seismic gap. Scientific Reports, 8(1), Makale 6819. https://doi.org/10.1038/s41598-018-23536-7

@article{9ecfd1ff8b8f4004bd9957816bef5b0c,

title = "Gas and seismicity within the Istanbul seismic gap",

abstract = "Understanding micro-seismicity is a critical question for earthquake hazard assessment. Since the devastating earthquakes of Izmit and Duzce in 1999, the seismicity along the submerged section of North Anatolian Fault within the Sea of Marmara (comprising the {"}Istanbul seismic gap{"}) has been extensively studied in order to infer its mechanical behaviour (creeping vs locked). So far, the seismicity has been interpreted only in terms of being tectonic-driven, although the Main Marmara Fault (MMF) is known to strike across multiple hydrocarbon gas sources. Here, we show that a large number of the aftershocks that followed the M 5.1 earthquake of July, 25th 2011 in the western Sea of Marmara, occurred within a zone of gas overpressuring in the 1.5-5 km depth range, from where pressurized gas is expected to migrate along the MMF, up to the surface sediment layers. Hence, gas-related processes should also be considered for a complete interpretation of the micro-seismicity (~M < 3) within the Istanbul offshore domain.",

author = "L. G{\'e}li and P. Henry and C. Grall and Tary, {J. B.} and A. Lomax and E. Batsi and V. Riboulot and E. Cros and C. G{\"u}rb{\"u}z and I{\c s}lk, {S. E.} and Seng{\"o}r, {A. M.C.} and {Le Pichon}, X. and L. Ruffine and S. Dupr{\'e} and Y. Thomas and D. Kalafat and G. Bayrakci and Q. Coutellier and T. Regnier and G. Westbrook and H. Saritas and G. {\c C}if{\c c}i and {\c C}aǧatay, {M. N.} and {\"O}zeren, {M. S.} and N. G{\"o}r{\"u}r and M. Tryon and M. Bohnhoff and L. Gasperini and F. Klingelhoefer and C. Scalabrin and Augustin, {J. M.} and D. Embriaco and G. Marinaro and F. Frugoni and S. Monna and G. Etiope and P. Favali and A. B{\'e}cel",

note = "Publisher Copyright: {\textcopyright} 2018 The Author(s).",

year = "2018",

month = dec,

day = "1",

doi = "10.1038/s41598-018-23536-7",

language = "English",

volume = "8",

journal = "Scientific Reports",

issn = "2045-2322",

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Géli, L, Henry, P, Grall, C, Tary, JB, Lomax, A, Batsi, E, Riboulot, V, Cros, E, Gürbüz, C, Işlk, SE, Sengör, AMC, Le Pichon, X, Ruffine, L, Dupré, S, Thomas, Y, Kalafat, D, Bayrakci, G, Coutellier, Q, Regnier, T, Westbrook, G, Saritas, H, Çifçi, G, Çaǧatay, MN, Özeren, MS, Görür, N, Tryon, M, Bohnhoff, M, Gasperini, L, Klingelhoefer, F, Scalabrin, C, Augustin, JM, Embriaco, D, Marinaro, G, Frugoni, F, Monna, S, Etiope, G, Favali, P & Bécel, A 2018, 'Gas and seismicity within the Istanbul seismic gap', Scientific Reports, hac. 8, no. 1, 6819. https://doi.org/10.1038/s41598-018-23536-7

TY - JOUR

T1 - Gas and seismicity within the Istanbul seismic gap

AU - Géli, L.

AU - Henry, P.

AU - Grall, C.

AU - Tary, J. B.

AU - Lomax, A.

AU - Batsi, E.

AU - Riboulot, V.

AU - Cros, E.

AU - Gürbüz, C.

AU - Işlk, S. E.

AU - Sengör, A. M.C.

AU - Le Pichon, X.

AU - Ruffine, L.

AU - Dupré, S.

AU - Thomas, Y.

AU - Kalafat, D.

AU - Bayrakci, G.

AU - Coutellier, Q.

AU - Regnier, T.

AU - Westbrook, G.

AU - Saritas, H.

AU - Çifçi, G.

AU - Çaǧatay, M. N.

AU - Özeren, M. S.

AU - Görür, N.

AU - Tryon, M.

AU - Bohnhoff, M.

AU - Gasperini, L.

AU - Klingelhoefer, F.

AU - Scalabrin, C.

AU - Augustin, J. M.

AU - Embriaco, D.

AU - Marinaro, G.

AU - Frugoni, F.

AU - Monna, S.

AU - Etiope, G.

AU - Favali, P.

AU - Bécel, A.

PY - 2018/12/1

Y1 - 2018/12/1

N2 - Understanding micro-seismicity is a critical question for earthquake hazard assessment. Since the devastating earthquakes of Izmit and Duzce in 1999, the seismicity along the submerged section of North Anatolian Fault within the Sea of Marmara (comprising the "Istanbul seismic gap") has been extensively studied in order to infer its mechanical behaviour (creeping vs locked). So far, the seismicity has been interpreted only in terms of being tectonic-driven, although the Main Marmara Fault (MMF) is known to strike across multiple hydrocarbon gas sources. Here, we show that a large number of the aftershocks that followed the M 5.1 earthquake of July, 25th 2011 in the western Sea of Marmara, occurred within a zone of gas overpressuring in the 1.5-5 km depth range, from where pressurized gas is expected to migrate along the MMF, up to the surface sediment layers. Hence, gas-related processes should also be considered for a complete interpretation of the micro-seismicity (~M < 3) within the Istanbul offshore domain.

AB - Understanding micro-seismicity is a critical question for earthquake hazard assessment. Since the devastating earthquakes of Izmit and Duzce in 1999, the seismicity along the submerged section of North Anatolian Fault within the Sea of Marmara (comprising the "Istanbul seismic gap") has been extensively studied in order to infer its mechanical behaviour (creeping vs locked). So far, the seismicity has been interpreted only in terms of being tectonic-driven, although the Main Marmara Fault (MMF) is known to strike across multiple hydrocarbon gas sources. Here, we show that a large number of the aftershocks that followed the M 5.1 earthquake of July, 25th 2011 in the western Sea of Marmara, occurred within a zone of gas overpressuring in the 1.5-5 km depth range, from where pressurized gas is expected to migrate along the MMF, up to the surface sediment layers. Hence, gas-related processes should also be considered for a complete interpretation of the micro-seismicity (~M < 3) within the Istanbul offshore domain.

UR - http://www.scopus.com/inward/record.url?scp=85046363781&partnerID=8YFLogxK

U2 - 10.1038/s41598-018-23536-7

DO - 10.1038/s41598-018-23536-7

M3 - Article

C2 - 29717139

AN - SCOPUS:85046363781

SN - 2045-2322

VL - 8

JO - Scientific Reports

JF - Scientific Reports

IS - 1

M1 - 6819

ER -

Gas and seismicity within the Istanbul seismic gap

Özet

Bibliyografik not

BM SKH

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