Pages that link to "Item:Q46550"

The following pages link to Jeanne Hardebeck (Q46550):

Displayed 50 items.

• Stress orientations at intermediate angles to the San Andreas Fault, California (Q144513) ‎ (← links)
• Temporal stress changes caused by earthquakes: A review (Q145233) ‎ (← links)
• Testing for the ‘predictability’ of dynamically triggered earthquakes in Geysers Geothermal Field (Q145235) ‎ (← links)
• Stress rotation across the Cascadia megathrust requires a weak subduction plate boundary at seismogenic depths (Q145277) ‎ (← links)
• The Mw6.0 24 August 2014 South Napa earthquake (Q148189) ‎ (← links)
• Preliminary report on the 22 December 2003, M 6.5 San Simeon, California earthquake (Q148390) ‎ (← links)
• Fracture-mesh faulting in the swarm-like 2020 Maacama sequence revealed by high-precision earthquake detection, location, and focal mechanisms (Q150096) ‎ (← links)
• Using machine learning techniques with incomplete polarity datasets to improve earthquake focal mechanism determination (Q150244) ‎ (← links)
• Physical properties of the crust influence aftershock locations (Q150522) ‎ (← links)
• Earthquakes in the shadows: Why aftershocks occur at surprising locations (Q150697) ‎ (← links)
• Aftershocks of the 2014 South Napa, California, Earthquake: Complex faulting on secondary faults (Q151672) ‎ (← links)
• A new strategy for earthquake focal mechanisms using waveform-correlation-derived relative polarities and cluster analysis: Application to the 2014 Long Valley Caldera earthquake swarm (Q153011) ‎ (← links)
• Three ingredients for Improved global aftershock forecasts: Tectonic region, time-dependent catalog incompleteness, and inter-sequence variability (Q153199) ‎ (← links)
• Complex faulting associated with the 22 December 2003 <i>M_w</i> 6.5 San Simeon California, earthquake, aftershocks and postseismic surface deformation (Q155358) ‎ (← links)
• The impact of static stress change, dynamic stress change, and the background stress on aftershock focal mechanisms (Q155818) ‎ (← links)
• Imaging shear strength along subduction faults (Q156170) ‎ (← links)
• Comment on “Models of stochastic, spatially varying stress in the crust compatible with focal‐mechanism data, and how stress inversions can be biased toward the stress rate” by Deborah Elaine Smith and Thomas H. Heaton (Q233818) ‎ (← links)
• Stress orientations in subduction zones and the strength of subduction megathrust faults (Q234439) ‎ (← links)
• A spatiotemporal clustering model for the Third Uniform California Earthquake Rupture Forecast (UCERF3‐ETAS): Toward an operational earthquake forecast (Q238809) ‎ (← links)
• The spatial distribution of earthquake stress rotations following large subduction zone earthquakes (Q239329) ‎ (← links)
• A synoptic view of the Third Uniform California Earthquake Rupture Forecast (UCERF3) (Q239540) ‎ (← links)
• Geometry and earthquake potential of the shoreline fault, central California (Q242682) ‎ (← links)
• Size distribution of Parkfield’s microearthquakes reflects changes in surface creep rate (Q242762) ‎ (← links)
• Seismicity around Parkfield correlates with static shear stress changes following the 2003 Mw6.5 San Simeon earthquake (Q243030) ‎ (← links)
• Fluid‐driven seismicity response of the Rinconada fault near Paso Robles, California, to the 2003 M 6.5 San Simeon earthquake (Q245502) ‎ (← links)
• Seismotectonics and fault structure of the California Central Coast (Q248293) ‎ (← links)
• Implications for prediction and hazard assessment from the 2004 Parkfield earthquake (Q250208) ‎ (← links)
• A stress-similarity triggering model for aftershocks of the MW6.4 and MW7.1 Ridgecrest earthquakes (Q253333) ‎ (← links)
• Toward a time-dependent probabilistic seismic hazard analysis for Alaska (Q254717) ‎ (← links)
• Earthquake stress drops and inferred fault strength on the Hayward Fault, east San Francisco Bay, California (Q258212) ‎ (← links)
• Precise tremor source locations and amplitude variations along the lower-crustal central San Andreas Fault (Q259642) ‎ (← links)
• Aftershock forecasting (Q262638) ‎ (← links)
• Does earthquake stress drop increase with depth in the crust? (Q264150) ‎ (← links)
• S/P amplitude ratios derived from single-component seismograms and their potential use in constraining focal mechanisms for micro-earthquake sequences (Q277856) ‎ (← links)
• Earth’s free surface complicates inference of absolute stress from earthquake-Induced stress rotations (Q281053) ‎ (← links)
• Prospective and retrospective evaluation of the U.S. Geological Survey public aftershock forecast for the 2019-2021 Southwest Puerto Rico Earthquake and aftershocks (Q282891) ‎ (← links)
• Localized fluid discharge by tensile cracking during the post-seismic period in subduction zones (Q288958) ‎ (← links)
• Coseismic and postseismic stress rotations due to great subduction zone earthquakes (Q291814) ‎ (← links)
• Are the stress drops of small earthquakes good predictors of the stress drops of moderate-to-large earthquakes? (Q292890) ‎ (← links)
• Developing earthquake forecast templates for fast and effective communication (Q294644) ‎ (← links)
• Earthquake recurrence models fail when earthquakes fail to reset the stress field (Q295181) ‎ (← links)
• Using corrected and imputed polarity measurements to improve focal mechanisms in a regional earthquake catalog near the Mt. Lewis Fault Zone, California (Q296162) ‎ (← links)
• Aftershocks are well aligned with the background stress field, contradicting the hypothesis of highly-heterogeneous crustal stress (Q297531) ‎ (← links)
• Seismicity rate changes along the central California coast due to stress changes from the 2003 M 6.5 San Simeon and 2004 M 6.0 Parkfield earthquakes (Q297767) ‎ (← links)
• A unified model of crustal stress heterogeneity from borehole breakouts and earthquake focal mechanisms (Q299924) ‎ (← links)
• Updated California aftershock parameters (Q307388) ‎ (← links)
• Spatial clustering of aftershocks impacts the performance of physics‐based earthquake forecasting models (Q309354) ‎ (← links)
• Supporting Data for "Subduction intraslab-interface fault interactions in the 2022 Mw 6.4 Ferndale, California, earthquake sequence" (Q319531) ‎ (← links)
• SKHASH: Python package for earthquake focal mechanism inversions (Q319601) ‎ (← links)
• High resolution earthquake relocations and focal mechanisms with preferred fault planes for the 2020 Maacama sequence (Q324258) ‎ (← links)