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Entertaining Geophysics 4. The Study of Seismic Phenomena as the Process of Fortune-Telling on the Coffee Grounds. What Does the School Curriculum Say about Earthquake Energy?
Seismic hazard from the Hispaniola subduction zone: Correction to “Historical perspective on seismic hazard to Hispaniola and the northeast Caribbean region”
Seismic dynamic and coseismic strains, distance decay rates, observation of major ruptures and propagation velocities of dynamic strain waves from high-rate GNSS with applications to the 2011 Tohoku Mw9.0 earthquake
Feature extraction and improved denoising method for nonlinear and nonstationary high-rate GNSS coseismic displacements applied to earthquake focal mechanism inversion of the El Mayor–Cucapah earthquake
Pre-seismic tilt rate variations and transient disturbances along the Longmenshan Fault Zone: Insights from continuous ground tilt data prior to the 2008 Wenchuan Earthquake
The dilatancy-diffusion hypothesis, earthquake prediction, and operational earthquake forecasting: In memory of Professor Amos Nur on the 50th Anniversary of the 1975 Haicheng Earthquake
The relationship between kinematics and fault geometry for surface coseismic ruptures on across-strike faults: New observations of slip vectors and displacements along the Pisia and Skinos faults from the 1981 Eastern Gulf of Corinth, Greece earthquakes
Long-term patterns of earthquakes influenced by climate change: Insights from earthquake recurrence and stress field changes across the Korean Peninsula during interglacial periods
Neotectonic faults in the Southern Chile intra-arc (38°S–40.5°S): Insights about their seismic potential and the link with the megathrust earthquake cycle
Identifying the fracture characteristics that control deformation localization and catastrophic failure in fluid-saturated crystalline rocks in upper crustal conditions
Postseismic deformation due to the M w 6.0 2004 Parkfield earthquake: Stress‐driven creep on a fault with spatially variable rate‐and‐state friction parameters
Inferring the coseismic and postseismic stress changes caused by the 2004 Mw = 6 Parkfield earthquake from variations of recurrence times of microearthquakes
Bilinearity in the Gutenberg‐Richter Relation Based on M L for Magnitudes Above and Below 2, From Systematic Magnitude Assessments in Parkfield (California)
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