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Current Issue

Volume 112,

Number 5,

October 2022

View This Issue

Impact Factor: 3.140 (37 of 87 in geochemistry/geophysics)

New Online

Late Pleistocene Slip Rate and 3D Geometry of the Mid‐Channel Blind Thrust, Santa Barbara Channel, California, and Their Implications for Earthquake Hazards

The Mechanisms of Tsunami Amplification and the Earthquake Source of the 2021 M 7 Acapulco, Mexico, Earthquake

Erratum to San Andreas Fault Earthquake Chronology and Lake Cahuilla History at Coachella, California

Erratum to Basin Amplification Effects in the Puget Lowland, Washington, from Strong‐Motion Recordings and 3D Simulations

The Geodetic Centroid (gCent) Catalog: Global Earthquake Monitoring with Satellite Imaging Geodesy

Behavior of Tidally Triggered Earthquakes Depends on Fluid Conditions

Small Seismic Events in Oklahoma Detected and Located by Machine Learning–Based Models

Reply to “Comment on ‘How Well Does Poissonian Probabilistic Seismic Hazard Assessment (PSHA) Approximate the Simulated Hazard of Epidemic‐Type Earthquake Sequences?’ by Shaoqing Wang, Maximilian J. Werner, and Ruifang Yu” by Iunio Iervolino, and Massimiliano Giorgio

Comment on “How Well Does Poissonian Probabilistic Seismic Hazard Assessment (PSHA) Approximate the Simulated Hazard of Epidemic‐Type Earthquake Sequences?” by Shaoqing Wang, Maximilian J. Werner, and Ruifang Yu

CALL FOR PAPERS

Click on the links below for more information about the issue, guest editors, submission deadlines, and publication dates.

SRL Special Section on Seismoacoustics and Seismoacoustic Data Fusion
Submission Deadline: 1 Nov 2022

Most Read
Most Cited

295 Construction of a Ground‐Motion Logic Tree through Host‐to‐Target Region Adjustments Applied to an Adaptable Ground‐Motion Prediction Model

276 New Insights on Subsurface Geology and the San Andreas Fault at Loma Prieta, Central California

242 Geostatistical Framework for Estimation of

V_{S 30}

in Data‐Scarce Regions

224 Shape Dynamic Time Warping for Seismic Waveform Inversion

221 Behavior of Tidally Triggered Earthquakes Depends on Fluid Conditions

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