Gas and seismicity within the Istanbul seismic gap.
Géli L, Henry P, Grall C, Tary JB, Lomax A, Batsi E, Riboulot V, Cros E, Gürbüz C, Işık 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, Çağatay 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.
Géli L, et al.
Sci Rep. 2018 May 1;8(1):6819. doi: 10.1038/s41598-018-23536-7.
Sci Rep. 2018.
PMID: 29717139
Free PMC article.
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 …
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 Ma …