M. Khoshmanesh
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View article: The 2020 Westmorland, California Earthquake Swarm as Aftershocks of a Slow Slip Event Sustained by Fluid Flow
The 2020 Westmorland, California Earthquake Swarm as Aftershocks of a Slow Slip Event Sustained by Fluid Flow Open
Swarms are bursts of earthquakes without an obvious mainshock. Some have been observed to be associated with transient aseismic fault slip, while others are thought to be related to fluids. However, the association is rarely quantitative d…
View article: Persistent impact of spring floods on crop loss in U.S. Midwest
Persistent impact of spring floods on crop loss in U.S. Midwest Open
View article: Surface Deformation and Seismicity Induced by Poroelastic Stress at the Raft River Geothermal Field, Idaho, USA
Surface Deformation and Seismicity Induced by Poroelastic Stress at the Raft River Geothermal Field, Idaho, USA Open
We investigate the relative importance of injection and production on the spatial‐temporal distribution of induced seismicity at the Raft River geothermal field. We use time‐series of InSAR measurements to document surface deformation and …
View article: Surface Deformation and Seismicity Induced by Poroelastic Stress at the Raft River Geothermal Field, Idaho, USA
Surface Deformation and Seismicity Induced by Poroelastic Stress at the Raft River Geothermal Field, Idaho, USA Open
Earth and Space Science Open Archive This work has been accepted for publication in Geophysical Research Letters. Version of RecordESSOAr is a venue for early communication or feedback before peer review. Data may be preliminary. Learn mor…
View article: Time Series Phase Unwrapping Based on Graph Theory and Compressed Sensing
Time Series Phase Unwrapping Based on Graph Theory and Compressed Sensing Open
Earth and Space Science Open Archive This preprint has been submitted to and is under consideration at Geophysical Research Letters. ESSOAr is a venue for early communication or feedback before peer review. Data may be preliminary.Learn mo…
View article: Deep slow-slip events promote seismicity in northeastern Japan megathrust
Deep slow-slip events promote seismicity in northeastern Japan megathrust Open
The sliding movement between oceanic and crustal plates in subduction zones is accommodated through both earthquakes and quasi-static or transient aseismic slip. On northeastern Japan megathrust, aseismic transients, known as slow-slip eve…
View article: Time-dependent investigation of a slow-moving landslide in Los Angeles, CA, through SAR observations and numerical simulations
Time-dependent investigation of a slow-moving landslide in Los Angeles, CA, through SAR observations and numerical simulations Open
<p>As urbanized areas increasingly expand into mountainous terrains and climate change accentuates extreme weather conditions (rainfall or drought), slow-moving landslides increasingly threaten the resilience of infrastructure system…
View article: Episodic creep events on the San Andreas Fault caused by pore pressure variations
Episodic creep events on the San Andreas Fault caused by pore pressure variations Open
View article: Time‐dependent model of aseismic slip on the central San Andreas Fault from InSAR time series and repeating earthquakes
Time‐dependent model of aseismic slip on the central San Andreas Fault from InSAR time series and repeating earthquakes Open
The Central segment of San Andreas Fault (CSAF) is characterized by a nearly continuous right‐lateral aseismic slip. However, observations of the creep rate obtained using small characteristically repeating earthquakes (CREs) show pulses o…