The geometry, length, and displacement of fault ruptures that breach the surface provide critical information on the behavior of faults during seismic events (coseismic deformation), and on their long-term behavior. The study of coseismic fault ruptures has concentrated almost exclusively along continental faults, while submarine studies have been scarce, and only a few provided quantitative constraints in parameters such as fault displacement (e.g., Tohoku Earthquake). In addition to represent more than two thirds of the Earth’s seismicity, submarine faults can also be associated with tsunamis, potentially increasing the seismic hazard that these structures pose.
During the ODEMAR 2013 cruise onboard N/O PourquoiPas? (IFREMER, FR) we used the autonomous underwater vehicle AUV Abyss (GEOMAR, D) and the remotely operated vehicle ROV VICTOR 6000 (IFREMER, FR) to map and survey the Roseau Fault between Guadeloupe et Dominica, in the Lesser Antilles, at water depths of ~1000 m. This fault ruptured during the 2004 Les Saintes Earthquake (magnitude 6.3), that also triggered a tsunami with a run-up of up to 3.5 m. The Roseau fault bounds an extensional intra-arc graben that accommodates extension perpendicular to the overall arc orientation. In this area a recent study based on extensive multi beam, sonar, and high-resolution seismic reflection profiles has documented complex fault interactions with submarine volcanism, erosion, and sedimentation.
The near-bottom, high resolution bathymetry and imagery acquired with the deep sea vehicles have allowed us to identify, for the first time, a marker of coseismic displacement along a normal submarine fault, that can be associated with the 2004 Les Saintes earthquake fault rupture. Coseismic displacement is observed along a ~20 m long sub-vertical fault surface, that is weathered and dusted with sediment, except for a ribbon at its base that is continuous and has a smooth, unweathered surface, that is likely exposed by the recent 2004 earthquake. A terrain model of this fault scarp constructed from ROV video imagery allows us to measure a displacement of 0.9 m. Seafloor photomosaics acquired during these surveys also reveal cracks in the sediments at the base of the fault scarp, documenting a damage zone that locally extends to >100 m off-fault. These deformation structures suggest that the Mw6.3 earthquake had a minimum surface rupture length of 3 km along the surveyed fault scarp, with a vertical displacement of ~1 m.
These results demonstrate that neotectonic studies using deep-sea vehicles for data acquisition, and state of the art imaging techniques (structure from motion, photomosaicing) for data processing, can now be conducted at the seafloor to obtain high-resolution data and observations comparable to those routinely acquired on-land. We will conduct in 2017 the SubSaintes cruise in this same area, to extend the mapping and geophysical observations from 2013. During this cruise we will deploy the ROV Victor6000 from the vessel NO Atalante. During this cruise we plan to extend the visual observations to other sub-vertical fault planes exposed along the base of the fault scarp, so as to quantify vertical displacement along the entire fault system.
These surveys will also determine if the unseuveyed fault ruptured beyond the 3 km that we have documented here. We will also extend our photomosaic surveys to thoroughly map deformation structures, and how these vary both along the fault and away from it. Finally, microbathymetry will be acquired throughout the area to study the interactions between volcanism and faulting. Sampling of faults and volcanic rocks will provide information on the nature of the fault rocks and style of weathering, and on the age and geochemical evolution of the volcanism in the area and their interactions with faults.
- Escartín, J., Leclerc, F., Olive, J., Mevel, C., Cannat, M., Petersen, S., Augustin, N., Feuillet, N., Deplus, C., Bezos, A., Bonnemains, D., Chavagnac, V., Choi, Y., Godard, M., Haaga, K.A., Hamelin, C., Ildefonse, B., Jamieson, J.W., John, B.E., Leleu, T., Macleod, C.J., Massot-campos, M., Nomikou, P., Paquet, M., Rommevaux-jestin, C., Rothenbeck, M., Steinführer, A., Tominaga, M., Triebe, L., Campos, R., Gracias, N., Garcia, R., Andreani, M., 2016. First direct observation of coseismic slip and seafloor rupture along a submarine normal fault and implications for fault slip history. Earth Planet. Sci. Lett. 450, 96–107.
Roseau Fault and regional tectonics
- Leclerc, F., N. Feuillet and C. Deplus, Interactions between active faulting, volcanism, and sedimentary processes at an island arc: Insights from Les Saintes channel, Lesser Antilles arc, DOI : 10.1002/2016GC006337, in press in G-cubed.
- Feuillet N., Beauducel F., Tapponnier P., 2011. The Mw = 6.3, November 21, 2004, Les Saintes earthquake (Guadeloupe): Tectonic setting, slip model and static stress changes. JGR, vol. 116.
- J. Escartín, IPGP, France: firstname.lastname@example.org
- F. Leclerc, EOS, Singapur: email@example.com
International & National Web Links – Paraskevi Nomikou | 2020-04-08|08:56 (UTC)
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