Results 131 to 140 of about 63,820 (273)
Datasets of disrupted transportation networks on Canada's West Coast in a plausible M9.0 Cascadia Subduction Zone earthquake scenario. [PDF]
Data Brief, 2023 Souza Almeida L +6 more
europepmc +1 more source
Geophysical Research Letters, Volume 53, Issue 4, 28 February 2026.Abstract Reconstructing oroclinal orogens along the Fuegian Andes‐northern Antarctic Peninsula provides critical constraints on the pre‐opening tectonic evolution of the Drake Passage, although such efforts are limited by a lack of reliable Cretaceous paleomagnetic and geochronological data.
Liang Gao +6 more
wiley +1 more source
Fluid pressurisation and earthquake propagation in the Hikurangi subduction zone. [PDF]
Nat Commun, 2021 Aretusini S +4 more
europepmc +1 more source
P‐Wave Reverberations in the Water Column of the Chilean Subduction Trench
Geophysical Research Letters, Volume 53, Issue 3, 16 February 2026.Abstract P‐waves generated by subduction earthquakes can get trapped within the submarine trench, where they reverberate and contaminate the initial seismic signals. We analyze the behavior of P‐wave reverberations for 43 earthquakes of magnitude larger than 6.0 that occurred along the Chilean margin between 1995 and 2023. We compared the energy of the
H. Schwarze, R. Madariaga, S. Ruiz
wiley +1 more source
3D anisotropic structure of the Japan subduction zone. [PDF]
Sci Adv, 2021 Wang Z, Zhao D.
europepmc +1 more source
Deep-water turbidites as Holocene earthquake proxies: the Cascadia subduction zone and Northern San Andreas Fault systems [PDF]
, 2003 New stratigraphic evidence from the Cascadia margin demonstrates that 13 earthquakes ruptured the margin from Vancouver Island to at least the California border following the catastrophic eruption of Mount Mazama.
Goldfinger, Chris +2 more
core +1 more source
Geophysical Research Letters, Volume 53, Issue 3, 16 February 2026.Abstract In this paper we document the first example‐the southern Delaware Basin‐where widespread induced triggered (as opposed to “driven”) seismicity across a large area exhibits a maximum magnitude truncation. The most likely cause of this truncation is that although the shallow faults in this area are many km in length, they are structurally ...
James P. Verdon, Ryan Schultz
wiley +1 more source
Effects of episodic slow slip on seismicity and stress near a subduction-zone megathrust. [PDF]
Nat Commun, 2021 Kita S +6 more
europepmc +1 more source
Geophysical Research Letters, Volume 53, Issue 3, 16 February 2026.Abstract Slow, aseismic fault slip has emerged as a significant contributor to the seismic cycle. However, whether slow and fast slip arise from similar physical processes remains unresolved, due to detection biases affecting noisy surface measurements and the analysis of the source properties of slow slip.
Giuseppe Costantino +3 more
wiley +1 more source
Relationship between tectonic tremors and 3-D distributions of thermal structure and dehydration in the Alaska subduction zone. [PDF]
Sci Rep, 2022 Iwamoto K, Suenaga N, Yoshioka S.
europepmc +1 more source