Phased Array Analysis Incorporating the Continuous Wavelet Transform

Calibrating the 2016 IRIS Wavefields Experiment Nodal Sensors for Amplitude Statics and Orientation Errors

Shallow Shear‐Wave Velocity Structure in Oklahoma Based on the Joint Inversion of Ambient Noise Dispersion and Teleseismic P ‐Wave Receiver Functions

Separating Signal from Noise and from Other Signal Using Nonlinear Thresholding and Scale‐Time Windowing of Continuous Wavelet Transforms

Automatic noise-removal/signal-removal based on general cross-validation thresholding in synchrosqueezed domain and its application on earthquake data

An Assessment of Crustal and Upper‐Mantle Velocity Structure by Removing the Effect of an Ice Layer on the P ‐Wave Response: An Application to Antarctic Seismic Studies

Velocity Structure of the Northern Mississippi Embayment Sediments, Part II: Inversion of Teleseismic P ‐Wave Transfer Functions

Velocity Structure of the Northern Mississippi Embayment Sediments, Part I: Teleseismic P ‐Wave Spectral Ratios Analysis

Small‐Scale Array Experiments in Seismic‐Wave Gradiometry

Imaging Shallow Crustal Structure in the Upper Mississippi Embayment Using Local Earthquake Waveform Data

Automatic microseismic denoising and onset detection using the synchrosqueezed continuous wavelet transform

Hybrid Seismic Denoising Using Higher‐Order Statistics and Improved Wavelet Block Thresholding

Vertical seismic wave gradiometry: Application at the San Andreas Fault Observatory at Depth

Local Magnitude and Anomalous Amplitude Distance Decay in the Eastern Tennessee Seismic Zone

Mysterious Tremor‐Like Signals Seen on the Reelfoot Fault, Northern Tennessee

Coherence of Teleseismic P and S waves across the Transportable Array

Three‐Dimensional Seismic‐Velocity Model for the Unconsolidated Mississippi Embayment Sediments from H/V Ambient Noise Measurements

Variation of Seismic b ‐Value in the New Madrid Seismic Zone: Evidence that the Northern Reelfoot Fault is Creeping

Wave-Field Continuation and Decomposition for Passive Seismic Imaging Under Deep Unconsolidated Sediments

Waveform Inversion for One-Dimensional Near-Surface Structure in the New Madrid Seismic Zone