Tectonophysics, ISSN 0040-1951, 01/2015, Volume 638, Issue 1, pp. 43 - 62
Understanding earthquake (EQ) recurrence relies on information about the timing and size of past EQ ruptures along a given fault. Knowledge of a fault's...
High-resolution topography | strike-slip faults | lidar | Earthquake recurrence models | slip accumulation pattern | Lidar | Strike-slip faults | Slip accumulation pattern | SAN-ANDREAS-FAULT | STRUCTURE-FROM-MOTION | SURFACE RUPTURE | CARRIZO-PLAIN | ALPINE FAULT | DEFORMATION | GEOCHEMISTRY & GEOPHYSICS | LANDERS EARTHQUAKE | SOUTHERN CALIFORNIA | MAYOR-CUCAPAH EARTHQUAKE | Strike-slip faults (Geology) | Earthquakes | Analysis | Optical radar | Faults | Geomorphology | Constraints | Slip | Constants | Time measurements | Coefficient of variation | Offsets | Seismic phenomena
High-resolution topography | strike-slip faults | lidar | Earthquake recurrence models | slip accumulation pattern | Lidar | Strike-slip faults | Slip accumulation pattern | SAN-ANDREAS-FAULT | STRUCTURE-FROM-MOTION | SURFACE RUPTURE | CARRIZO-PLAIN | ALPINE FAULT | DEFORMATION | GEOCHEMISTRY & GEOPHYSICS | LANDERS EARTHQUAKE | SOUTHERN CALIFORNIA | MAYOR-CUCAPAH EARTHQUAKE | Strike-slip faults (Geology) | Earthquakes | Analysis | Optical radar | Faults | Geomorphology | Constraints | Slip | Constants | Time measurements | Coefficient of variation | Offsets | Seismic phenomena
Journal Article
Geophysical Journal International, ISSN 0956-540X, 09/2011, Volume 186, Issue 3, pp. 897 - 927
SUMMARY We carried out morphotectonic studies along the left‐lateral strike‐slip Bogd Fault, the principal structure involved in the Gobi‐Altay earthquake of...
Geomorphology | Seismic cycle | Continental neotectonics | Asia | Continental tectonics: strike‐slip and transform | Earthquake dynamics | Continental tectonics: strike-slip and transform | HALF-LIFE | SYSTEM | RANGE GOBI-ALTAY | BEHAVIOR | ALTYN-TAGH FAULT | EXAMPLES | SITU-PRODUCED BE-10 | GEOCHEMISTRY & GEOPHYSICS | LUMINESCENCE | AVERAGE RATE | LATE PLEISTOCENE | Earthquakes | Seismology | Analysis | Neotectonics | Tectonics (Geology) | Faults | Horizontal | Slip | Segments | Estimates | Offsets | Seismic phenomena | Tectonics | Earth Sciences | Sciences of the Universe
Geomorphology | Seismic cycle | Continental neotectonics | Asia | Continental tectonics: strike‐slip and transform | Earthquake dynamics | Continental tectonics: strike-slip and transform | HALF-LIFE | SYSTEM | RANGE GOBI-ALTAY | BEHAVIOR | ALTYN-TAGH FAULT | EXAMPLES | SITU-PRODUCED BE-10 | GEOCHEMISTRY & GEOPHYSICS | LUMINESCENCE | AVERAGE RATE | LATE PLEISTOCENE | Earthquakes | Seismology | Analysis | Neotectonics | Tectonics (Geology) | Faults | Horizontal | Slip | Segments | Estimates | Offsets | Seismic phenomena | Tectonics | Earth Sciences | Sciences of the Universe
Journal Article
Geophysical Research Letters, ISSN 0094-8276, 09/2017, Volume 44, Issue 17, pp. 8749 - 8756
Slow slip phenomena, including earthquake afterslip and discrete slow slip events (SSEs), may have a major effect on megathrust earthquakes in subduction...
afterslip | friction experiment | slip‐dependent weakening | JFAST | slow slip | The 2011 Tohoku‐Oki earthquake | The 2011 Tohoku-Oki earthquake | slip-dependent weakening | VELOCITY | GEOSCIENCES, MULTIDISCIPLINARY | LOW-FREQUENCY EARTHQUAKES | OKI EARTHQUAKE | ROCK FRICTION | ZONE | JAPAN | PARAMETERS | EVENT | MEXICO | Fault zones | Seismic activity | Subduction zones | Friction | Subduction (geology) | Earthquakes | Slip | Velocity | Plate boundaries | Subduction
afterslip | friction experiment | slip‐dependent weakening | JFAST | slow slip | The 2011 Tohoku‐Oki earthquake | The 2011 Tohoku-Oki earthquake | slip-dependent weakening | VELOCITY | GEOSCIENCES, MULTIDISCIPLINARY | LOW-FREQUENCY EARTHQUAKES | OKI EARTHQUAKE | ROCK FRICTION | ZONE | JAPAN | PARAMETERS | EVENT | MEXICO | Fault zones | Seismic activity | Subduction zones | Friction | Subduction (geology) | Earthquakes | Slip | Velocity | Plate boundaries | Subduction
Journal Article
Geophysical Research Letters, ISSN 0094-8276, 05/2018, Volume 45, Issue 9, pp. 3880 - 3888
Detailed new paleoseismic field investigations at two sites on the Talas‐Fergana fault, a poorly known strike‐slip structure that transects the Tien Shan...
Tien Shan | India‐Asia tectonics | seismic hazard | Talas‐Fergana slip rate | lithosphere behavior | Talas-Fergana slip rate | India-Asia tectonics | TIEN-SHAN | GEOSCIENCES, MULTIDISCIPLINARY | TECTONICS | SAN-ANDREAS FAULT | CENTRAL-ASIA | EARTHQUAKE-CYCLE | COLLISION | ALTYN TAGH FAULT | MODEL | DEFORMATION | STRAIN | Seismic activity | Variability | Slip | Seismic hazard | Contraction | Remote sensing | Fault lines | Geological faults | Orogeny | Earthquakes | Temporal variability | Global positioning systems--GPS | Field tests | Positioning systems | Temporal variations | Plate tectonics | Palaeo studies | Plates (tectonics) | Geology | Lithosphere | Data | Global Positioning System | Satellites | Hazard assessment | Geological hazards | Holocene
Tien Shan | India‐Asia tectonics | seismic hazard | Talas‐Fergana slip rate | lithosphere behavior | Talas-Fergana slip rate | India-Asia tectonics | TIEN-SHAN | GEOSCIENCES, MULTIDISCIPLINARY | TECTONICS | SAN-ANDREAS FAULT | CENTRAL-ASIA | EARTHQUAKE-CYCLE | COLLISION | ALTYN TAGH FAULT | MODEL | DEFORMATION | STRAIN | Seismic activity | Variability | Slip | Seismic hazard | Contraction | Remote sensing | Fault lines | Geological faults | Orogeny | Earthquakes | Temporal variability | Global positioning systems--GPS | Field tests | Positioning systems | Temporal variations | Plate tectonics | Palaeo studies | Plates (tectonics) | Geology | Lithosphere | Data | Global Positioning System | Satellites | Hazard assessment | Geological hazards | Holocene
Journal Article
Geochemistry, Geophysics, Geosystems, ISSN 1525-2027, 12/2014, Volume 15, Issue 12, pp. 5034 - 5050
Comparison of 398 fault offsets measured by visual analysis of WorldView high‐resolution satellite imagery with deformation maps produced by COSI‐Corr subpixel...
strain localization | near‐surface materials | Balochistan earthquake | structural maturity | off‐fault deformation | fault slip rates | near-surface materials | off-fault deformation | Structural maturity | Fault slip rates | Near-surface materials | Strain localization | Off-fault deformation | DIFFERENTIAL LIDAR | SUBPIXEL CORRELATION | TURKEY | DEFICIT | DENALI | GEOCHEMISTRY & GEOPHYSICS | ACCRETIONARY WEDGE | CALIFORNIA | RUPTURE | NOVEMBER 1999 DUZCE | MAYOR-CUCAPAH EARTHQUAKE | Earthquakes | Deformation
strain localization | near‐surface materials | Balochistan earthquake | structural maturity | off‐fault deformation | fault slip rates | near-surface materials | off-fault deformation | Structural maturity | Fault slip rates | Near-surface materials | Strain localization | Off-fault deformation | DIFFERENTIAL LIDAR | SUBPIXEL CORRELATION | TURKEY | DEFICIT | DENALI | GEOCHEMISTRY & GEOPHYSICS | ACCRETIONARY WEDGE | CALIFORNIA | RUPTURE | NOVEMBER 1999 DUZCE | MAYOR-CUCAPAH EARTHQUAKE | Earthquakes | Deformation
Journal Article
Pure and Applied Geophysics, ISSN 0033-4553, 9/2019, Volume 176, Issue 9, pp. 3975 - 3992
In order to explain the seismic–aseismic slip patterns observed on megathrust faults, numerical simulations were carried out using the quasi-dynamic asperity...
Earth Sciences | Earthquake dynamics | subduction zone processes | slow and fast slip | Geophysics/Geodesy | slip-dependent friction | megathrust earthquakes | numerical modeling | ZONE | SUBDUCTION | MODEL | GEOCHEMISTRY & GEOPHYSICS | SHEAR | EARTHQUAKE CYCLE | AREA | SEAMOUNTS | RUPTURE | DYNAMICS | FAULTS | Numerical simulations | Parameters | Computer simulation | Seismic activity | Subduction (geology) | Rupture | Fronts | Slip | Subduction | Geological faults | Friction | Earthquakes | Stiffness | Mathematical models | Distance | Seamounts | Free surfaces | Asperity
Earth Sciences | Earthquake dynamics | subduction zone processes | slow and fast slip | Geophysics/Geodesy | slip-dependent friction | megathrust earthquakes | numerical modeling | ZONE | SUBDUCTION | MODEL | GEOCHEMISTRY & GEOPHYSICS | SHEAR | EARTHQUAKE CYCLE | AREA | SEAMOUNTS | RUPTURE | DYNAMICS | FAULTS | Numerical simulations | Parameters | Computer simulation | Seismic activity | Subduction (geology) | Rupture | Fronts | Slip | Subduction | Geological faults | Friction | Earthquakes | Stiffness | Mathematical models | Distance | Seamounts | Free surfaces | Asperity
Journal Article
Geophysical Research Letters, ISSN 0094-8276, 09/2011, Volume 38, Issue 18, p. n/a
Episodic Tremor and Slip (ETS), involving transient deformations accompanied by emergent, low‐frequency tremor occurs in subduction zones around the world. ETS...
slow slip | subduction zone | SUBDUCTION ZONE | GEOSCIENCES, MULTIDISCIPLINARY | EARTHQUAKES | EPISODIC TREMOR | JAPAN | Geodetics | Seismology | Plate tectonics | Rock deformation | Faults | Correlation | Slip | Satellite navigation systems | Creep (materials) | Tremors | Global Positioning System | Asperity
slow slip | subduction zone | SUBDUCTION ZONE | GEOSCIENCES, MULTIDISCIPLINARY | EARTHQUAKES | EPISODIC TREMOR | JAPAN | Geodetics | Seismology | Plate tectonics | Rock deformation | Faults | Correlation | Slip | Satellite navigation systems | Creep (materials) | Tremors | Global Positioning System | Asperity
Journal Article
Science, ISSN 0036-8075, 06/2015, Volume 348, Issue 6240, pp. 1224 - 1226
Anthropogenic fluid injections are known to induce earthquakes. The mechanisms involved are poorly understood, and our ability to assess the seismic hazard...
FAULT ZONE | EARTHQUAKE | FRICTION LAWS | MULTIDISCIPLINARY SCIENCES | Seismic reflection method | Models | Seismic waves | Methods | Geological faults | Friction | Earthquakes | Slip | Fluid injection | Monitoring | Seismicity | Waste water | Earth Sciences | Sciences of the Universe
FAULT ZONE | EARTHQUAKE | FRICTION LAWS | MULTIDISCIPLINARY SCIENCES | Seismic reflection method | Models | Seismic waves | Methods | Geological faults | Friction | Earthquakes | Slip | Fluid injection | Monitoring | Seismicity | Waste water | Earth Sciences | Sciences of the Universe
Journal Article
Earth and Planetary Science Letters, ISSN 0012-821X, 02/2014, Volume 388, pp. 38 - 47
Comparisons of observed surface displacements with geodetically inferred slip at depth in six large ( ) strike-slip earthquakes reveal a correlation between...
strain localization | comparison of geologic and geodetic rate data | strain transient | probabilistic seismic hazard assessment | fault slip rates | structural evolution of faults | Strain transient | Comparison of geologic and geodetic rate data | Fault slip rates | Strain localization | Probabilistic seismic hazard assessment | Structural evolution of faults | NORTH ANATOLIAN FAULT | MOJAVE DESERT | GROUND MOTION | TURKEY | CALIFORNIA SHEAR ZONE | GEOCHEMISTRY & GEOPHYSICS | TRANSIENT STRAIN ACCUMULATION | RUPTURE | 1999 HECTOR MINE | ASYMMETRIC DAMAGE | DENALI-FAULT | Measurement | Earthquakes | Seismology | Analysis | Faults | Geological faults | Geology | Slip | Rupture | Offsets | Seismic phenomena
strain localization | comparison of geologic and geodetic rate data | strain transient | probabilistic seismic hazard assessment | fault slip rates | structural evolution of faults | Strain transient | Comparison of geologic and geodetic rate data | Fault slip rates | Strain localization | Probabilistic seismic hazard assessment | Structural evolution of faults | NORTH ANATOLIAN FAULT | MOJAVE DESERT | GROUND MOTION | TURKEY | CALIFORNIA SHEAR ZONE | GEOCHEMISTRY & GEOPHYSICS | TRANSIENT STRAIN ACCUMULATION | RUPTURE | 1999 HECTOR MINE | ASYMMETRIC DAMAGE | DENALI-FAULT | Measurement | Earthquakes | Seismology | Analysis | Faults | Geological faults | Geology | Slip | Rupture | Offsets | Seismic phenomena
Journal Article
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Full Text
Rapid automated W‐phase slip inversion for the Illapel great earthquake (2015, Mw = 8.3)
Geophysical Research Letters, ISSN 0094-8276, 03/2016, Volume 43, Issue 5, pp. 1910 - 1917
We perform rapid W‐phase finite fault inversion for the 2015 Illapel great earthquake (Mw = 8.3). To evaluate the performance of the inversion in a near real...
W‐phase | finite fault modeling | earthquake source inversion | early warning | W-phase | GEOSCIENCES, MULTIDISCIPLINARY | MODELS | UNCERTAINTY | TSUNAMI | FAULT SLIP | Earthquakes | Seismology | Plate tectonics | Methodology | Slip | Emergency management | Emergencies | Inversion | Management | Surveying | Real time | Emergency warning programs | Geological surveys | Mathematical analysis | Seismic surveys | Emergency preparedness | Tsunamis
W‐phase | finite fault modeling | earthquake source inversion | early warning | W-phase | GEOSCIENCES, MULTIDISCIPLINARY | MODELS | UNCERTAINTY | TSUNAMI | FAULT SLIP | Earthquakes | Seismology | Plate tectonics | Methodology | Slip | Emergency management | Emergencies | Inversion | Management | Surveying | Real time | Emergency warning programs | Geological surveys | Mathematical analysis | Seismic surveys | Emergency preparedness | Tsunamis
Journal Article
Journal of Geophysical Research: Solid Earth, ISSN 0148-0227, 04/2010, Volume 115, Issue B4, p. n/a
We invert for the time‐dependent slip history of slow slip events on the Cascadia subduction zone using GPS data from 1998 to 2008. The 16 slip transients have...
Cascadia | aseismic slip | GEOCHEMISTRY & GEOPHYSICS | SOUTHWEST JAPAN | REPEATING EARTHQUAKES | EPISODIC TREMOR | SILENT SLIP | STRESS | FAULT SLIP | DEFORMATION | MODULATION | Seismology | Rock deformation | Continental dynamics | Geophysics | Geodetics | Marine geology | Plate tectonics | Stations | Correlation | Slip | Satellite navigation systems | Boundaries | Strikes | Global Positioning System | Geographic information systems
Cascadia | aseismic slip | GEOCHEMISTRY & GEOPHYSICS | SOUTHWEST JAPAN | REPEATING EARTHQUAKES | EPISODIC TREMOR | SILENT SLIP | STRESS | FAULT SLIP | DEFORMATION | MODULATION | Seismology | Rock deformation | Continental dynamics | Geophysics | Geodetics | Marine geology | Plate tectonics | Stations | Correlation | Slip | Satellite navigation systems | Boundaries | Strikes | Global Positioning System | Geographic information systems
Journal Article
Geophysical Research Letters, ISSN 0094-8276, 02/2015, Volume 42, Issue 4, pp. 1113 - 1121
We investigate the influence of elastic heterogeneity on geodetic inversions of slow‐slip events by inverting for slip distributions of four events along the...
geodetic inversion | subduction zones | elastic heterogeneity | slow‐slip events | slip budgets | slow-slip events | SEISMIC STRUCTURE | GEOSCIENCES, MULTIDISCIPLINARY | NEW-ZEALAND | TENSILE FAULTS | MODELS | ZONE | HALF-SPACE | HIKURANGI MARGIN | EARTHQUAKES | DEFORMATION | NORTH-ISLAND | Estimates | Heterogeneity | Offshore | Half spaces | Mathematical analysis | Slip | Geophysics | Inversions | Mathematical models
geodetic inversion | subduction zones | elastic heterogeneity | slow‐slip events | slip budgets | slow-slip events | SEISMIC STRUCTURE | GEOSCIENCES, MULTIDISCIPLINARY | NEW-ZEALAND | TENSILE FAULTS | MODELS | ZONE | HALF-SPACE | HIKURANGI MARGIN | EARTHQUAKES | DEFORMATION | NORTH-ISLAND | Estimates | Heterogeneity | Offshore | Half spaces | Mathematical analysis | Slip | Geophysics | Inversions | Mathematical models
Journal Article