The Horseshoe Abyssal plain Thrust could be the source of the 1755 Lisbon earthquake and tsunami

Autor: Sara Martínez-Loriente, Valentí Sallarès, Eulàlia Gràcia

Publikováno v: Communications Earth & Environment, Vol 2, Iss 1, Pp 1-9 (2021)

The 1755 Great Lisbon earthquake potentially had its source on the Horseshoe Abyssal plain Thrust, southwest of Iberia, according to a comparison of geophysical observations, historical reports and numerical modelling of the tsunami that was generate

Externí odkaz: https://doaj.org/article/2827b66f10f646c4b72d7598b53cd2d8

Earthquake crisis unveils the growth of an incipient continental fault system

Autor: Eulàlia Gràcia, Ingo Grevemeyer, Rafael Bartolomé, Hector Perea, Sara Martínez-Loriente, Laura Gómez de la Peña, Antonio Villaseñor, Yann Klinger, Claudio Lo Iacono, Susana Diez, Alcinoe Calahorrano, Miquel Camafort, Sergio Costa, Elia d’Acremont, Alain Rabaute, César R. Ranero

Publikováno v: Nature Communications, Vol 10, Iss 1, Pp 1-12 (2019)

The Al-Idrissi Fault System in the Alboran Sea is a major tectonic structure in its initial stage. By using bathymetric and seismic reflection data, the authors unravel a 3D geometry for the AIFS, which corresponds to a crustal-scale boundary and pro

Externí odkaz: https://doaj.org/article/cfc4cc0e5a8b48838ab6227e22de5d9b

Seafloor expression of the deep structure during initiation of transtensional fault systems, as seen in the North-South fault system of the Alboran Sea, SE Iberia

Autor: Eulàlia Gràcia, David Fernández-Blanco, Hector Perea, Sara Martínez-Loriente, Jaume Llopart, Ariadna Canari

How fault segments grow and connect in regions with moderate to high seismic activity is key to assess associated hazards. Earthquakes may affect populated areas and can trigger tsunamis that threaten coastal areas and affect marine infrastructures.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d4689e1453a51151fc52352e74164828
https://doi.org/10.5194/egusphere-egu22-514

Tectonic evolution, geomorphology and influence of bottom currents along a large submarine canyon system: The São Vicente Canyon (SW Iberian margin)

Autor: Rafael Bartolomé, Alexis Vizcaino, Claudio Lo Iacono, Juanjo Dañobeitia, Nevio Zitellini, S. Diez, Eulàlia Gràcia, Héctor Perea, Cristina Sanchez Serra, Roger Urgeles, Pedro Terrinha, Raimon Pallàs, Sara Martínez-Loriente

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
Universidad Pontificia Comillas ICAI-ICADE
Marine geology
426 (2020). doi:10.1016/j.margeo.2020.106219
info:cnr-pdr/source/autori:S. Serra C.; Martinez-Loriente S.; Gracia E.; Urgeles R.; Vizcaino A.; Perea H.; Bartolome R.; Pallas R.; Lo Iacono C.; Diez S.; Danobeitia J.; Terrinha P.; Zitellini N./titolo:Tectonic evolution, geomorphology and influence of bottom currents along a large submarine canyon system: The São Vicente Canyon (SW Iberian margin)/doi:10.1016%2Fj.margeo.2020.106219/rivista:Marine geology (Print)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:426

16 pages, 11 figures, 1 table, supplementary data https://doi.org/10.1016/j.margeo.2020.106219
A multi-scale dataset consisting of multi-beam echo-sounder, 2D multi-channel seismic and sidescan sonar (TOBI) data allows us to identify a large var

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::558084456f5ee6457401747103c9ea05

Revealing the earthquake history during the last 200 ka on a large submarine strike-slip fault: The Yusuf Fault System (Alboran Sea)

Autor: Rafael Bartolomé, Eulàlia Gràcia, L. Gómez de la Peña, Stefanie Almeida, Sara Martínez-Loriente, Héctor Perea

Publikováno v: Digital.CSIC. Repositorio Institucional del CSIC
instname

European Geosciences Union (EGU) General Assembly 2020, 4-8 May 2020
The NW-SE convergence (4-5 mm/yr) between the African and Eurasian plates controls the present-day crustal deformation in the Alboran Sea (westernmost Mediterranean). Although

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::783c4b348757d278805ac82a5e79b943
http://hdl.handle.net/10261/225530