Area of research
Geophysics
Research interest
Research interests include Geology, Seismology, Mantle (geology), Subduction, Mars Exploration Program, and Crust.
Urban dark fiber distributed acoustic sensing for bridge monitoring
Marsquake Locations and 1‐D Seismic Models for Mars From InSight Data
Basaltic reservoirs in the Earth’s mantle transition zone
Thickness and structure of the martian crust from InSight seismic data
A poorly mixed mantle transition zone and its thermal state inferred from seismic waves
Improving Constraints on Planetary Interiors With PPs Receiver Functions
Potential Pitfalls in the Analysis and Structural Interpretation of Seismic Data from the Mars <i>InSight</i> Mission
Autocorrelation of the Ground Vibrations Recorded by the SEIS‐InSight Seismometer on Mars
Seismic Noise Autocorrelations on Mars
Automatic Identification of Mantle Seismic Phases Using a Convolutional Neural Network
Constraints on the shallow elastic and anelastic structure of Mars from InSight seismic data
Seismological evidence for thermo-chemical heterogeneity in Earth's continental mantle
Multifrequency Inversion of Ps and Sp Receiver Functions: Methodology and Application to USArray Data
Crust stratigraphy and heterogeneities of the first kilometers at the dichotomy boundary in western Elysium Planitia and implications for InSight lander
Receiver functions from seismic interferometry: a practical guide
Pervasive seismic low-velocity zones within stagnant plates in the mantle transition zone: Thermal or compositional origin?
Pervasive upper mantle melting beneath the western US
Cascadia subduction slab heterogeneity revealed by three‐dimensional receiver function Kirchhoff migration
Multi-mode conversion imaging of the subducted Gorda and Juan de Fuca plates below the North American continent
Deep crustal fracture zones control fluid escape and the seismic cycle in the Cascadia subduction zone
Seismically deduced thermodynamics phase diagrams for the mantle transition zone
Multiple transition zone seismic discontinuities and low velocity layers below western United States
Seismoacoustic coupling induced by the breakup of the 15 February 2013 Chelyabinsk meteor
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