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Collot Jean-Yves, Sanclemente E., Nocquet Jean-Mathieu, Lepretre A., Ribodetti Alessandra, Jarrin P., Chlieh Mohamed, Graindorge D., Charvis Philippe. (2017). Subducted oceanic relief locks the shallow megathrust in central Ecuador. Journal of Geophysical Research : Solid Earth, 122 (5), 3286-3305. ISSN 2169-9313

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Lien direct chez l'éditeur doi:10.1002/2016jb013849

Titre
Subducted oceanic relief locks the shallow megathrust in central Ecuador
Année de publication2017
Type de documentArticle référencé dans le Web of Science WOS:000403465600002
AuteursCollot Jean-Yves, Sanclemente E., Nocquet Jean-Mathieu, Lepretre A., Ribodetti Alessandra, Jarrin P., Chlieh Mohamed, Graindorge D., Charvis Philippe.
SourceJournal of Geophysical Research : Solid Earth, 2017, 122 (5), p. 3286-3305. ISSN 2169-9313
RésuméWhether subducted oceanic reliefs such as seamounts promote seismic rupture or aseismic slip remains controversial. Here we use swath bathymetry, prestack depth-migrated multichannel seismic reflection lines, and wide-angle seismic data collected across the central Ecuador subduction segment to reveal a broad similar to 55kmx50km, similar to 1.5-2.0km high, low height-to-width ratio, multipeaked, sediment-bare, shallow subducted oceanic relief. Owing to La Plata Island and the coastline being located, respectively, similar to 35km and similar to 50-60km from the trench, GPS measurements allow us to demonstrate that the subducted oceanic relief spatially correlates to a shallow, similar to 80kmx55km locked interplate asperity within a dominantly creeping subduction segment. The oceanic relief geometrical anomaly together with its highly jagged topography, the absence of a subduction channel, and a stiff erosive oceanic margin are found to be long-term geological characteristics associated with the shallow locking of the megathrust. Although the size and level of locking observed at the subducted relief scale could produce an M-w >7+ event, no large earthquakes are known to have happened for several centuries. On the contrary, frequent slow slip events have been recorded since 2010 within the locked patch, and regular seismic swarms have occurred in this area during the last 40years. These transient processes, together with the rough subducted oceanic topography, suggest that interplate friction might actually be heterogeneous within the locked patch. Additionally, we find that the subducted relief undergoes internal shearing and produces a permanent flexural bulge of the margin, which uplifted La Plata Island. Plain Language Summary Subducted seamounts play an important but still uncertain role in earthquake rupture processes, as seamounts are considered to subduct either aseismically or seismically. We use marine geophysical data across the central Ecuador convergent margin to reveal a broad similar to 55kmx50km, similar to 1.5-2.0km high, shallow subducted oceanic relief of the Carnegie Ridge. New GPS measurements collected on La Plata Island and along the Ecuador coast allow us to demonstrate that the subducted oceanic relief spatially correlates to a shallow, similar to 80kmx55km locked interplate asperity within a dominantly creeping subduction segment. The oceanic relief geometrical anomaly together with its rough topography and the stiff oceanic Ecuador margin are found to be long-term geological characteristics associated with the shallow locking of the plate interface. Although the size and level of locking observed at the subducted relief scale could produce an M-w >7+ event, no large earthquake but frequent slow slip events and associated seismic swarms occurred within the locked patch. These transient processes together with the rough subducted oceanic topography support the view of a heterogeneous interplate frictional pattern within the locked patch. On a regional scale, the subduction of the oceanic relief has deformed the Ecuador margin and uplifted La Plata Island.
Plan de classementGéophysique interne [066]
Descr. géo.EQUATEUR ; ANDES ; PACIFIQUE ; LA PLATA ILE
LocalisationFonds IRD [F B010070238]
Identifiant IRDfdi:010070238
Lien permanenthttp://www.documentation.ird.fr/hor/fdi:010070238

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