Publications des scientifiques de l'IRD

van Rijsingen E. M., Calais Eric, Jolivet R., De Chabalier J. B., Robertson R., Ryan G. A., Symithe S. (2022). Ongoing tectonic subsidence in the Lesser Antilles subduction zone. Geophysical Journal International, 231 (1), 319-326. ISSN 0956-540X.

Titre du document
Ongoing tectonic subsidence in the Lesser Antilles subduction zone
Année de publication
2022
Type de document
Article référencé dans le Web of Science WOS:000814811100003
Auteurs
van Rijsingen E. M., Calais Eric, Jolivet R., De Chabalier J. B., Robertson R., Ryan G. A., Symithe S.
Source
Geophysical Journal International, 2022, 231 (1), 319-326 ISSN 0956-540X
Geological estimates of vertical motions in the central part of the Lesser Antilles show subsidence on timescales ranging from 125.000 to 100 yr, which has been interpreted to be caused by interseismic locking along the subduction megathrust. However, horizontal GNSS velocities show that the Lesser Antilles subduction interface is currently building up little to no elastic strain. Here, we present new present-day vertical velocities for the Lesser Antilles islands and explore the link between short- and long-term vertical motions and their underlying processes. We find a geodetic subsidence of the Lesser Antilles island arc at 1-2 mm yr(-1), consistent with the similar to 100-yr trend derived from coral micro-atolls. Using elastic dislocation models, we show that a locked or partially locked subduction interface would produce uplift of the island arc, opposite to the observations, hence supporting a poorly coupled subduction. We propose that this long-term, margin-wide subsidence is controlled by slab dynamic processes, such as slab rollback. Such processes could also be responsible for the aseismic character of the subduction megathrust.
Plan de classement
Géologie et formations superficielles [064] ; Géophysique interne [066]
Description Géographique
PETITES ANTILLES
Localisation
Fonds IRD [F B010085322]
Identifiant IRD
fdi:010085322
Contact