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<datestamp>2018-01-11</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>Which fault destroyed Fes city (Morocco) in 1755? A new insight from the Holocene deformations observed along the southern border of Gibraltar arc</title>
<creator>Poujol, Antoine</creator>
<creator>RITZ, Jean-francois</creator>
<creator>VERNANT, Philippe</creator>
<creator>Huot, Sebastien</creator>
<creator>Maate, Soufian</creator>
<creator>Tahayt, Abdelilah</creator>
<contributor>National Central University, Taoyuan</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Risques ; Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS) - Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>University of Illinois, Urbana-Champaign</contributor>
<contributor>Université Mohammed V, Rabat</contributor>
<description>International audience</description>
<source>ISSN: 0040-1951</source>
<source>EISSN: 1879-3266</source>
<source>Tectonophysics</source>
<publisher>Elsevier</publisher>
<identifier>hal-01622048</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-01622048</identifier>
<source>https://hal.archives-ouvertes.fr/hal-01622048</source>
<source>Tectonophysics, Elsevier, 2017, 712, pp.303-311. 〈10.1016/j.tecto.2017.05.036〉</source>
<identifier>DOI : 10.1016/j.tecto.2017.05.036</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1016/j.tecto.2017.05.036</relation>
<language>en</language>
<subject lang=en>"1755" earthquake</subject>
<subject lang=en>Surface rupture</subject>
<subject lang=en>Rif (Morocco)</subject>
<subject lang=en>Morphotectonics</subject>
<subject lang=en>OSL</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>In this paper, we present the first estimate of the Holocene deformation along the southern front of Gibraltar arc (Morocco) and the first field constraints on the local 1755 CE Fes-Meknes surface rupturing earthquake which could be associated to the “Great Lisbon Earthquake” (M > 8.5) in November 1st, 1755. Using satellite imagery, aerial photographs and field investigations, we carried out a morphotectonic study along the ~ 150 km-long Southern Rif Front (SRF) to identify the most recent evidences of tectonic activity. Analyzed offset alluvial deposits confirm that (i) the last ~ 5 ka cumulative deformation leading to a slip rate of ~ 3.5 ± 1 mm/yr for this segment of the SRF is consistent with the GPS derived horizontal shortening rate of 2–4 mm/yr and (ii) a recent major earthquake ruptured a ~ 30 km-long segment along the SRF. Based on deposits dating and historical seismicity we propose that this seismic event occurred in 1755 as a local earthquake. Even though this 1755 local event cannot be considered as a strong aftershock of the main Lisbon seismic event (M > 8.5), their temporal closeness, their occurrence under the same convergent stress regime (~ NNW-SSE-oriented compression) and the fact that Fes-Meknes area was strongly shaken during the Lisbon earthquake, raises the question of the possible triggering of the Fes earthquake. Anyway, our new results suggest that most of the Nubia-Rif belt convergence is accommodated by the SRF, making it potentially the most destructive structure of the Rif.</description>
<date>2017-08-21</date>
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