DeerLab: a comprehensive software package for analyzing dipolar electron paramagnetic resonance spectroscopy data

L Fábregas Ibáñez, G Jeschke, S Stoll - Magnetic Resonance, 2020 - mr.copernicus.org
Dipolar electron paramagnetic resonance (EPR) spectroscopy (DEER and other techniques)
enables the structural characterization of macromolecular and biological systems by …

Simultaneous multitrace impedance inversion with transform-domain sparsity promotion

S Yuan, S Wang, C Luo, Y He - Geophysics, 2015 - library.seg.org
The impedance inversion technique plays a crucial role in seismic reservoir properties
prediction. However, most existing impedance inversion methods often suffer from spatial …

A balanced combination of Tikhonov and total variation regularizations for reconstruction of piecewise-smooth signals

A Gholami, SM Hosseini - Signal Processing, 2013 - Elsevier
This paper introduces a novel method to combine total variation and ℓ2 regularizations to
reconstruct piecewise smooth signals. The main idea is to consider the signal as a sum of …

Regularization of linear and non-linear geophysical ill-posed problems with joint sparsity constraints

A Gholami, HR Siahkoohi - Geophysical Journal International, 2010 - academic.oup.com
In this paper, we deal with the solution of linear and non-linear geophysical ill-posed
problems by requiring the solution to have sparse representations in two appropriate …

Computation of differential seismograms and iteration adaptive regularization in prestack waveform inversion

MK Sen, IG Roy - Geophysics, 2003 - pubs.geoscienceworld.org
Seismic waveform inversion is a highly challenging task. Nonlinearity, nonuniqueness, and
robustness issues tend to make the problem computationally intractable. We have …

Inferring the subsurface geometry and strength of slow‐moving landslides using 3‐D velocity measurements from the NASA/JPL UAVSAR

AL Handwerger, AM Booth, MH Huang… - Journal of …, 2021 - Wiley Online Library
The hazardous impact and erosive potential of slow‐moving landslides depends on
landslide properties including velocity, size, and frequency of occurrence. However …

Forward and inverse self-potential modeling in mineral exploration

CA Mendonça - Geophysics, 2008 - library.seg.org
Natural self-potential (SP) fields observed in the vicinity of conductive orebodies can be
explained in terms of electrochemical reactions in which the conductors participate. Battery …

The point-spread function measure of resolution for the 3-D electrical resistivity experiment

GA Oldenborger, PS Routh - Geophysical Journal International, 2009 - academic.oup.com
The solution appraisal component of the inverse problem involves investigation of the
relationship between our estimated model and the actual model. However, full appraisal is …

Nonlinear 3D tomographic least-squares inversion of residual moveout in Kirchhoff prestack-depth-migration common-image gathers

F Adler, R Baina, MA Soudani, P Cardon, JB Richard - Geophysics, 2008 - library.seg.org
Velocity-model estimation with seismic reflection tomography is a nonlinear inverse
problem. We present a new method for solving the nonlinear tomographic inverse problem …

Multi-scale reasonable attenuation tomography analysis (MuRAT): An imaging algorithm designed for volcanic regions

L De Siena, C Thomas, R Aster - Journal of Volcanology and Geothermal …, 2014 - Elsevier
The attenuation of body-wave amplitudes with propagation distance can be used to provide
detailed tomographic images of seismic interfaces, fluid reservoirs, and melt batches in the …