Temporal stress changes caused by earthquakes: A review

JL Hardebeck, T Okada - Journal of Geophysical Research …, 2018 - Wiley Online Library
Earthquakes can change the stress field in the Earth's lithosphere as they relieve and
redistribute stress. Earthquake‐induced stress changes have been observed as temporal …

Stress map of Japan: Detailed nationwide crustal stress field inferred from focal mechanism solutions of numerous microearthquakes

T Uchide, T Shiina, K Imanishi - Journal of Geophysical …, 2022 - Wiley Online Library
Crustal stress is a crucial parameter for understanding tectonics and assessing the
occurrence of large earthquakes. Stress at seismogenic depths over a wide area has been …

Recent advances in characterizing the crustal stress field and future applications of stress data: Perspectives from North America

JE Lundstern - Geological Society, London, Special Publications, 2024 - lyellcollection.org
The stress field controls patterns of crustal deformation, including which faults are likeliest to
cause earthquakes or transmit fluids. Since the 1950s, maps of maximum horizontal stress …

Focal mechanisms of small earthquakes beneath the Japanese islands based on first-motion polarities picked using deep learning

T Uchide - Geophysical Journal International, 2020 - academic.oup.com
Knowledge of crustal stress fields is essential for understanding tectonics and earthquake
generation. One approach for estimating the crustal stress field is based on the focal …

[HTML][HTML] Neotectonic transpressional intraplate deformation in eastern Eurasia: Insights from active fault systems in the southeastern Korean Peninsula

N Kim, SI Park, CS Cho, Y Cheon, AL Peace - Geoscience Frontiers, 2023 - Elsevier
Transpression occurs in response to oblique convergence across a deformation zone in
intraplate regions and plate boundaries. The Korean Peninsula is located at an intraplate …

Hypocenter migration and seismicity pattern change in the Yamagata‐Fukushima border, NE Japan, caused by fluid movement and pore pressure variation

K Yoshida, A Hasegawa - Journal of Geophysical Research …, 2018 - Wiley Online Library
The spatiotemporal distributions of hypocenters and temporal change in seismicity patterns
were investigated in details for events in the Yamagata‐Fukushima border earthquake …

Temporal changes in stress drop, frictional strength, and earthquake size distribution in the 2011 Yamagata‐Fukushima, NE Japan, earthquake swarm, caused by …

K Yoshida, T Saito, Y Urata, Y Asano… - … Research: Solid Earth, 2017 - Wiley Online Library
In this study, we investigated temporal variations in stress drop and b‐value in the
earthquake swarm that occurred at the Yamagata‐Fukushima border, NE Japan, after the …

Stable forearc stressed by a weak megathrust: Mechanical and geodynamic implications of stress changes caused by the M= 9 Tohoku‐oki earthquake

K Wang, L Brown, Y Hu, K Yoshida… - Journal of Geophysical …, 2019 - Wiley Online Library
Rupture‐zone averaged static stress drop in the 2011 M= 9 Tohoku‐Oki earthquake was
less than 5 MPa, but it caused a stress reversal in most of the offshore forearc, although the …

Present‐day crustal stress field in Greece inferred from regional‐scale damped inversion of earthquake focal mechanisms

KI Konstantinou, V Mouslopoulou… - Journal of …, 2017 - Wiley Online Library
In this study we utilize regional and teleseismic earthquake moment tensor solutions in order
to infer the contemporary crustal stress in the Greek region. We focus on crustal earthquakes …

Heterogeneities in stress and strength in Tohoku and its relationship with earthquake sequences triggered by the 2011 M9 Tohoku-Oki earthquake

K Yoshida, A Hasegawa, T Yoshida… - Pure and Applied …, 2019 - Springer
Inland Tohoku has been recognized as under the WNW-ESE compressional stress state
before the 2011 M9 Tohoku-Oki earthquake. Earthquakes that occurred there were …