Estimating interseismic deformation in subduction fault zones can offer insights into the frequency and magnitude of megathrust earthquakes. Diffusive mass transfer is a significant …
Y Wu, J Liao, F Guo, XC Wang… - Geophysical Research …, 2022 - Wiley Online Library
Distinct signatures are present in the circum‐Pacific continental margins (eg, kinematics, magmatism, and basin evolution), possibly influenced by the input of mid‐ocean ridge. It …
Abstract The Shimanto Belt in SW Japan is commonly described as a paleo‐accretionary prism, whose structure is explained by continuous accretion like in modern accretionary …
H Hara, Y Nakamura, K Hara, T Kurihara, H Mori… - Island Arc, 2017 - Wiley Online Library
Detrital zircon multi‐chronology combined with provenance and low‐grade metamorphism analyses enables the reinterpretation of the tectonic evolution of the C retaceous S himanto …
H Raimbourg, K Rajič, B Moris‐Muttoni… - Geochemistry …, 2021 - Wiley Online Library
In several examples of subduction zones, we compared pairs of quartz veins formed either at the lower temperatures of the seismogenic zone (260° C or below), or at the higher …
Recent geophysical monitoring of subduction zones has unraveled a complete spectrum of plate coupling behaviors, from coupled portions rupturing during earthquakes to decoupled …
H Raimbourg, M Vacelet, C Ramboz, V Famin… - Tectonophysics, 2015 - Elsevier
Accretionary prisms constitute ideal targets to study fluid circulation and fluid–rock interactions at depths beyond the reach of active margin deep drilling. The highest-grade …
A Paleozoic subduction complex dominates the Mossman Orogen developed at the northern extremity of the Tasmanides, eastern Australia. Its southern part, displayed in the Broken …
In order to constrain deformation processes close to the brittle-ductile transition in seismogenic zone, we have carried out a microstructural study in the Shimanto accretionary …