The earthquake sequence, with a maximum earthquake magnitude of MW 3.8, that occurred during January–February 2022 at the northern Dead Sea fault, is shown to be induced by …
I Kurzon, RN Nof, M Laporte… - Seismological …, 2020 - pubs.geoscienceworld.org
Following the recommendations of an international committee, since October 2017, the Israeli Seismic Network has been undergoing significant upgrades, with 120 stations being …
A Inbal, A Ziv, I Lior, RN Nof… - Geophysical Research …, 2023 - Wiley Online Library
Most aftershocks occur in areas experiencing large co‐seismic stress changes, yet some occur long after the mainshock in remote lightly stressed regions. The triggering mechanism …
Y Hamiel, O Piatibratova - Journal of Geophysical Research …, 2021 - Wiley Online Library
Crustal deformation and seismic activity in the Levant is mainly related to the interplate Dead Sea Fault (DSF) and the intraplate Carmel–Gilboa Fault System (CGFS). In this study, we …
S Engelberg, A Sagy, R Shaar, A Matmon, AJ Hidy… - Tectonophysics, 2024 - Elsevier
Abstract The Gulf of Elat-Aqaba (GEA), located in the southern part of the Dead Sea Transform (DST), is one of the most active segments of the Dead Sea fault system. Yet, some …
Abstract The Sea of Galilee (Lake Kinneret) is located in northern Israel in a complex tectonic setting where the Dead Sea Transform crosscuts other fault systems. The practical …
O Barnea Cohen, S Cesca, T Dahm, A Hofstetter… - …, 2022 - Wiley Online Library
Abstract In October 2013 and July–August 2018, two extensive earthquake swarms shook the northern reaches of Lake Kinneret (Sea of Galilee). Former studies explored the swarms …
V Frid, A Rabinovitch, D Bahat, U Kushnir - Remote Sensing, 2023 - mdpi.com
This paper deals with the quantitative analysis of measured fracture-induced electromagnetic radiation (FEMR) near the Dead Sea Transform using the Angel-M1 …
Bends and stepovers in strike-slip fault systems along active plate boundaries are widespread and introduce stress heterogeneities, affecting the regional strain field. The …