Results 51 to 60 of about 11,312,720 (157)
A devastating earthquake with moment magnitude 7.5 occurred in the Noto Peninsula in central Japan on 1 January 2024. We estimate the rupture evolution of this earthquake from teleseismic P‐wave data using the potency‐density tensor inversion method ...
Ryo Okuwaki +3 more
doaj +1 more source
Overall-slow and dissipative rupture during the 2025 MW 7.1 Dingri, China earthquake
On 7 January 2025, the MW 7.1 Dingri earthquake in China ruptured a nearly north-south-trending normal-faulting fault within the southern Tibetan Plateau.
Xu Zhang +3 more
doaj +1 more source
The Mw8.4 Illapel earthquake occurred on 16 September was the largest global event in 2015. This earthquake was not unexpected because the hypocenter was located in a seismic gap of the Peru‐Chile subduction zone. However, the source model derived from 3‐
Shiann‐Jong Lee +5 more
doaj +1 more source
This article describes the results of a ground motion modeling study of the 1915 Avezzano earthquake. The goal was to test assuinptions regarding the rupture process of this earthquake by attempting to model the damage to historical monuments and ...
G. Longhi +5 more
doaj +1 more source
Short-period rupture process of the 2010 Mw 8.8 maule earthquake in Chile
International audienceThe 2010 Maule earthquake is one of the largest events ever recorded with modern instruments. We used the continuous GPS (cGPS) records to invert for the kinematic rupture process using an elliptical sub-patch approximation.
Ruiz, S. +6 more
core +1 more source
An M JMA 6.5 crustal earthquake occurred during earthquake swarm activity around the northeastern tip of the Noto Peninsula, central Japan, on May 5, 2023.
Kimiyuki Asano, Tomotaka Iwata
doaj +1 more source
Two-stage rupture during the Mw 8.3 Okhotsk 2013 deep-focus earthquake constrains slab geometry
The Mw 8.3 deep-focus earthquake beneath the Okhotsk Sea in 2013 provides an opportunity to study the source mechanism with regard to the specific geometry of the slab in the hypocentral region.
Ruohan Zhang +3 more
doaj +1 more source
Objective The coseismic surface rupture formed by an earthquake is the most obvious geomorphological evidence of fault activity. Its spatial distribution and deformation characteristics record essential information about seismic ruptures and fault ...
LIU Fucai +6 more
doaj +1 more source
The Mw7.8 2016 Kaikōura earthquake
We provide a summary of the surface fault ruptures produced by the Mw7.8 14 November 2016 Kaikōura earthquake, including examples of damage to engineered structures, transportation networks and farming infrastructure produced by direct fault surface ...
Sauer, K +56 more
core +1 more source
Exceptionally Elongated Strike‐Slip Rupture Caused by the 2025 MW 7.8 Myanmar Earthquake
The interplay between fault geometry and rupture behavior remains poorly understood. The 2025 Myanmar earthquake ruptured the Sagaing fault, a major continental strike‐slip fault with simple geometry.
Quanshu Zhao +7 more
doaj +1 more source

