Results 61 to 70 of about 238,525 (137)
Evolution of Scaled Energy During Earthquake Ruptures
Abstract Earthquake ruptures radiate seismic energy in complex ways, reflecting the interplay of fault heterogeneity and rupture dynamics. How the radiated energy evolves during rupture, and whether this evolution varies systematically with earthquake properties, remains poorly understood. Here we analyze more than 1,500 global earthquakes using moment‐
Binhao Wang, Heidi Houston
wiley +1 more source
The shallow slip deficit (SSD) during strike-slip earthquakes raises a question of how the strain budget is accommodated over multiple cycles. However, the origin of variable SSD observed in different earthquakes is still under debate because each ...
Zhen Li, Chenglong Li, Teng Wang
doaj +1 more source
Study on deformation characteristics and dynamic cause of the Luding MS6.8 earthquake
A MS6.8 earthquake struck Luding Country in Ganzi Prefecture, Sichuan Province on 5 September 2022. The earthquake occurred on the Moxi segment of Xianshuihe fault zone (XFZ), one of the most seismically active faults in the Chinese mainland.
Zhengyi Yuan +6 more
doaj +1 more source
Abstract Quantifying fault frictional properties is fundamental to understanding slip behavior and seismic hazard. We analyze 2 years of Sentinel‐1 SAR data following the 2023 Turkey earthquake doublet using Independent Component Analysis‐enhanced Small Baseline Subset‐InSAR, to resolve postseismic deformation and invert for afterslip on the East ...
Jianlong Chen +4 more
wiley +1 more source
Abstract The Alpine Fault (AF) in Aotearoa New Zealand is a fast‐slipping plate boundary fault late in its seismic cycle that presents a major source of seismic hazard. Past earthquakes have created a structural‐geomorphic record of surface ruptures that we map and analyze for the northern AF using 1,000 km2 ${\text{km}}^{2}$ of Light Detection and ...
J. La Greca +5 more
wiley +1 more source
On May 22, 2021, Mw 7.4 Maduo earthquake occurred in Qinhai province, China, which is located on Kunlunshankou-Jiangcuo fault China. In this paper, two type of the coseismic deformation of Maduo are reached using (interferometric synthetic aperture radar)
Jiaojiao Liu +6 more
core +1 more source
Geodetic Strain Rates, Slip Deficit Rates, and Seismic Potential in the Tianshan, Central Asia
Abstract The Tianshan is an intracontinental orogenic belt that has experienced over 100 Mw ≥ 6 earthquakes since 1700. However, strain rates and slip deficit rates on mapped faults in this region—key factors in assessing its seismic potential—remain underexplored.
Fengnian Chang +6 more
wiley +1 more source
Abstract We present high‐resolution rupture imaging of the 2025 MW 7.7 Myanmar earthquake using global teleseismic P‐waves and regional‐distance Rayleigh waves. Most radiated energy was released near the epicenter within the first 20 s, followed by bilateral rupture propagation along the central Sagaing Fault, extending ∼350 km southward and ∼100 km ...
Qiang Yao, Chunquan Yu, Min Zhou
wiley +1 more source
Earthquakes are environmental disturbances affecting ecosystem functioning, health, and biodiversity, but their potential impacts on plant–soil interface are still poorly understood.
Hui Zuo +15 more
doaj +1 more source
Abstract The amount and spatial distribution of surface displacement that occurs during an earthquake are critical information to the understanding of the earthquake source and rupture processes. However, the earthquake surface displacement occurs over wide regions, includes multiple components that affect the ground surface at different spatial scales,
Solène L. Antoine, Zhen Liu
wiley +1 more source

