Fault rupture and stress changes associated with the November 27, 2005 Qeshm Island (Iran) earthquake (MW = 6.0)
Author:
Funder
Sakarya Üniversitesi
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
http://link.springer.com/article/10.1007/s12517-018-4090-5/fulltext.html
Reference58 articles.
1. Alinaghi A (2007) Moment tensor inversion of some events of Qeshm island earthquake sequences using INSN broadband data. J Seismol Earthq Eng JSEE 9(3):153–157
2. Allen MB, Talebian M (2011) Structural variation along the Zagros and the nature of the Dezful embayment. Geol Mag 148(5–6):911–924. https://doi.org/10.1017/S0016756811000318
3. Allen MB, Saville C, Blanc EJ-P, Talebian M, Nissen E (2013) Orogenic plateau growth: expansion of the Turkish-Iranian plateau across the Zagros fold-and-thrust belt. Tectonics 32:171–190. https://doi.org/10.1002/tect.20025
4. Amighpey M, Voosoghi B, Motagh M (2014) Deformation and fault parameters of the 2005 Qeshm earthquake in Iran revisited: a Bayesian simulated annealing approach applied to the inversion of space geodetic data. Int J Appl Earth Obs Geoinf 26:184–192
5. Barnhart WD, Lohman RB (2013) Phantom earthquakes and triggered aseismic creep: vertical partitioning of strain during earthquake sequences in Iran. Geophys Res Lett 40:819–823. https://doi.org/10.1002/grl.50201
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1. Decoupled co-seismic deformation and stress changes during the 2021 (Mw 6.0, 6.4) North Bandar Abbas doublet earthquakes in Fin region, SE-syntaxis of Zagros, Iran: new insights into the tectonic deformation decoupling process;Environmental Earth Sciences;2023-10-26
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3. Coseismic slip distributions and stress interactions of the November 12, 2017, Sarpole-Zahab (Western Iran) earthquake (MW=7.3) and its aftershocks: seismotectonic implications;Arabian Journal of Geosciences;2021-06
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