Morphostructure, tectono-sedimentary evolution and seismic potential of the Horseshoe Fault, SW Iberian Margin.

Martinez-Loriente, S., Gracia, E., Bartolome, R., Perea, H., Klaeschen, Dirk, Danobeitia, J. J., Zitellini, N., Wynn, R. B. and Masson, D. G. (2018) Morphostructure, tectono-sedimentary evolution and seismic potential of the Horseshoe Fault, SW Iberian Margin. Basin Research, 30 (S1). pp. 382-400. DOI 10.1111/bre.12225.

[img] Text
Martinez-Loriente.pdf - Accepted Version
Restricted to Registered users only

Download (3571Kb) | Contact

Supplementary data:

Abstract

High-resolution acoustic and seismic data acquired 100 km offshore Cape São Vicente, image with unprecedented detail one of the largest active reverse faults of the SW Iberian Margin, the Horseshoe Fault (HF). The HF region is an area seismogenically active, source of the largest magnitude instrumental and historical earthquake (Mw>6) occurred in the SW Iberian Margin. The HF corresponds to a N40 trending, 110 km long, and NW-verging active thrust that affects the whole sedimentary sequence and reaches up to the seafloor, generating a relief of more than 1 km. The along-strike structural variability as well as fault trend suggests that the HF is composed by three main sub-segments: North (N25), Central (N50) and South (N45). Swath-bathymetry, TOBI sidescan sonar backscatter and parametric echosounder TOPAS profiles reveal the surface morphology of the HF block, characterized by several, steep (20º) small scarps located on the hangingwall, and a succession of mass transport deposits (i.e. turbidites) on its footwall, located in the Horseshoe Abyssal Plain. A succession of pre-stack depth-migrated multichannel seismic reflection profiles across the HF and neighboring areas allowed us to constrain their seismo-stratigraphy, structural geometry, tectono-sedimentary evolution from Upper Jurassic to present-day, and to calculate their fault parameters. Finally, on the basis of segment length, surface fault area and seismogenic depth we evaluated the seismic potential of the HF, which in the worst-case scenario may generate an earthquake of magnitude Mw 7.8 ± 0.1. Thus, considering the tectonic behavior and near-shore location, the HF should be recognized in seismic and tsunami hazard assessment models of Western Europe and North Africa.

Document Type: Article
Additional Information:
Keywords: Swath-bathymetry; TOBI sidescan sonar; multichannel seismic reflection; thrusts fault; strike-slip fault; seismic and tsunami hazard; Iberia-Africa plate boundary; RSS James Cook; JC027; RV Hesperides
Research affiliation: NOC
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1111/bre.12225
ISSN: 0950-091X
Projects: EVENT, SHAKE, INSIGHT, SWIM, SALVADORE, NEAREST, Future Ocean, FLOWS
Date Deposited: 30 Nov 2016 07:44
Last Modified: 17 Jan 2019 13:37
URI: http://oceanrep.geomar.de/id/eprint/34968

Actions (login required)

View Item View Item

Document Downloads

More statistics for this item...