Along-Trench Structural Variations of the Subducting Juan de Fuca Plate From Multichannel Seismic Reflection Imaging - INSU - Institut national des sciences de l'Univers Accéder directement au contenu
Article Dans Une Revue Journal of Geophysical Research : Solid Earth Année : 2018

Along-Trench Structural Variations of the Subducting Juan de Fuca Plate From Multichannel Seismic Reflection Imaging

Shuoshuo Han
  • Fonction : Auteur
Suzanne M. Carbotte
  • Fonction : Auteur
Juan Pablo Canales
  • Fonction : Auteur
Mladen R. Nedimović
  • Fonction : Auteur
Hélène Carton

Résumé

To characterize the along-strike structural variations of the Juan de Fuca (JdF) Plate as it enters the Cascadia subduction zone, we present prestack time migrated multichannel seismic reflection images of the JdF Plate along a 400-km-long trench-parallel transect extending from 44.3°N to 47.8°N. Beneath the 1.8-3.0-km-thick sediment cover, our data reveal basement topographic anomalies associated with a 1.2-km-high seamount and in the vicinity of propagator wakes (390-540-m relief). Weak Moho reflections are imaged beneath the propagator wakes and coincide with reduced Vp in the lower crust and/or uppermost mantle. The inferred locations of propagator wakes in the downgoing plate collocate with some of the boundaries of episodic tremor and slip events. We propose that the structural and hydration heterogeneities associated with these features could lead to anomalous plate interface properties and contribute to episodic tremor and slip segmentation. Intracrustal reflections with apparent dips (20°-30°) consistent with subduction bending normal faults change near 45.8°N, from northward dipping reflections confined to the middle crust in the north to antithetic reflections through the crust in the south, coinciding with a Vp reduction in the lower crust. These observations indicate more extensive faulting deformation and associated hydration of the JdF Plate south of 45.8°N, which likely results from variations of slab dip and resistance to subduction across 46°N. Basement offsets and abrupt depth/amplitude changes in Moho reflections are imaged beneath the four major WNW trending strike-slip faults that cross the Cascadia deformation front, providing strong evidence of a lower plate origin for these faults.
Fichier principal
Vignette du fichier
JGR Solid Earth - 2018 - Han - Along%u2010Trench Structural Variations of the Subducting Juan de Fuca Plate From Multichannel.pdf (17.33 Mo) Télécharger le fichier
Origine : Fichiers éditeurs autorisés sur une archive ouverte

Dates et versions

insu-03589359 , version 1 (25-02-2022)

Licence

Copyright (Tous droits réservés)

Identifiants

Citer

Shuoshuo Han, Suzanne M. Carbotte, Juan Pablo Canales, Mladen R. Nedimović, Hélène Carton. Along-Trench Structural Variations of the Subducting Juan de Fuca Plate From Multichannel Seismic Reflection Imaging. Journal of Geophysical Research : Solid Earth, 2018, 123, pp.3122-3146. ⟨10.1002/2017JB015059⟩. ⟨insu-03589359⟩
22 Consultations
8 Téléchargements

Altmetric

Partager

Gmail Facebook X LinkedIn More