William Frank is an Assistant Professor in the Department of Earth, Atmospheric and Planetary Sciences at the Massachusetts Institute of Technology. He leads the Tectonophysics research group that focuses on crustal deformation within the solid Earth, whether it’s the result of earthquakes or the slow shear of slow slip.
Latest
- Deep learning detects uncataloged low-frequency earthquakes across regions
- Low-Frequency Earthquakes Downdip of Deep Slow Slip Beneath the North Island of New Zealand
- Untangling the environmental and tectonic drivers of the Noto earthquake swarm in Japan
- BPMF: A backprojection and matched-filtering workflow for automated earthquake detection and location
- Along-strike segmentation of seismic tremor and its relationship with the hydraulic structure of the subduction fault zone
- Imaging the Spatiotemporal Evolution of Plate Coupling With Interferometric Radar (InSAR) in the Hikurangi Subduction Zone
- What makes low-frequency earthquakes low frequency
- Subdaily slow fault slip dynamics captured by low-frequency earthquakes
- Capturing seismic velocity changes in receiver functions with optimal transport
- A recursive matched-filter to systematically explore a volcanic long-period earthquake swarm
- Crustal structure across the West Antarctic rift system from multicomponent ambient noise surface wave tomography
- Tracking the Spatio-Temporal Evolution of Foreshocks Preceding the Mw 6.1 2009 L’Aquila Earthquake
- An adaptable random forest model for the declustering of earthquake catalogs
- Crust and upper-mantle seismic anisotropy variations from the coast to inland in central and Southern Mexico (2): Correlations with Tectonic Tremor
- Illuminating the Pre-, Co-, and Post-Seismic Phases of the 2016 M7.8 Kaikōura Earthquake With 10 Years of Seismicity
- Moment-duration scaling of low-frequency earthquakes in Guerrero, Mexico
- Statistical evidence of a seismic quiescence before the M$_w$8.1 Iquique earthquake, Chile
- The transient and intermittent nature of slow slip
- Daily measurement of slow slip from low-frequency earthquakes is consistent with ordinary earthquake scaling
- Systematic Detection of Clustered Seismicity Beneath the Southwestern Alps
- Isolated Triggered Tremor Spots in South America: Southern Chile, Ecuador, and Central Colombia
- Characteristic tectonic tremor activity observed over multiple slow slip cycles in the Mexican subduction zone
- Updip and along-strike aftershock migration model driven by afterslip: application to the 2011 Tohoku-Oki aftershock sequence
- Revealing the cluster of slow transients behind a large slow slip event
- Progressive reactivation of the volcanic plumbing system beneath Tolbachik volcano (Kamchatka, Russia) revealed by long-period seismicity
- A model for migration of aftershocks driven by afterslip
- Adapting the matched-filter search to a wide-aperture network: an aftershock sequence and an earthquake swarm in Connecticut
- Fast matched-filter (FMF): an efficient seismic matched-filter search for both CPU and GPU architectures
- Imbricated slip rate processes during slow slip transients imaged by low-frequency earthquakes
- A geodetic matched-filter search for slow slip with application to the Mexico subduction zone
- Mapping the rheology of the Central Chile subduction zone with aftershocks
- Repeating seismicity in the shallow crust modulated by transient stress perturbations
- Slow slip hidden in the noise: the intermittence of tectonic release
- The evolving interaction of low-frequency earthquakes during transient slip
- Spatial-temporal variation of low-frequency earthquake bursts near Parkfield, California
- Uncovering the geodetic signature of silent slip through repeating earthquakes
- Along-fault pore-pressure evolution during a slow-slip event in Guerrero, Mexico
- Using systematically characterized low-frequency earthquakes as a fault probe in Guerrero, Mexico
- Automatic detection of low-frequency earthquakes (LFEs) based on a beamformed network response
- Low-frequency earthquakes in the Mexican Sweet Spot