Papers

(2019) J. Araujo, André L. A. Reis, A. A. P. Correa, E. Yokoyama, Vanderlei C. Oliveira Jr., L. A. F. Mendoza, M. A. C. Pacheco, C. Luz-Lima, A. F. Santos, F. G. Osorio G., G. E. Brito, W. W. R. Araujo, Tahir, A. C. Bruno, T. Del Rosso. Materials.

Fast 3D magnetic inversion of a surface relief in the space domain

(2019) Marlon C. Hidalgo-Gato, Valéria C. F. Barbosa. Geophysics.

Gravitational field calculation in spherical coordinates using variable densities in depth

(2019) Santiago Soler, Agustina Pesce, Mario E. Gimenez, Leonardo Uieda. Geophysical Journal International.

Characterizing complex mineral structures in thin sections of geological samples with a scanning Hall effect microscope

(2019) J. Araujo, André L. A. Reis, Vanderlei C. Oliveira Jr., A. F. Santos, C. Luz-Lima, E. Yokoyama, L. A. F. Mendoza, J. M. B Pereira, A. C. Bruno. Sensors.

Efficient 3D large-scale forward-modeling and inversion of gravitational fields in spherical coordinates with application to lunar mascons

(2019) Guangdong Zhao, Bo Chen, Leonardo Uieda, Jianxin Liu, Mikhail K. Kaban, Longwei Chen, Rongwen Guo. Journal of Geophysical Research: Solid Earth.

How two gravity-gradient inversion methods can be used to reveal different geologic features of ore deposit — A case study from the Quadrilátero Ferrífero (Brazil)

(2016) Dionísio Uendro Carlos, Leonardo Uieda, Valéria C. F. Barbosa. Journal of Applied Geophysics.

Papers

Convolutional equivalent layer for magnetic data processing

Analyzing the Ambiguity of the Remanent-Magnetization Direction Separated Into Induced and Remanent Magnetic Sources

Magnetic radial inversion for 3-D source geometry estimation

Amplitude of the magnetic anomaly vector in the interpretation of total-field anomaly at low magnetic latitudes

Magnetic amplitude inversion for depth-to-basement and apparent magnetization-intensity estimates

Convolutional equivalent layer for gravity data processing

Generalized positivity constraint on magnetic equivalent layers

Gradient based first- and second-order filters for the demarcation of continental–oceanic boundaries using satellite gravity data

Reliable Euler deconvolution estimates throughout the vertical derivatives of the total-field anomaly

Isostatic constraint for 2D non-linear gravity inversion on rifted margins

Scanning magnetic microscope using a gradiometric configuration for characterization of rock samples

Fast 3D magnetic inversion of a surface relief in the space domain

Gravitational field calculation in spherical coordinates using variable densities in depth

Characterizing complex mineral structures in thin sections of geological samples with a scanning Hall effect microscope

Efficient 3D large-scale forward-modeling and inversion of gravitational fields in spherical coordinates with application to lunar mascons

Verde: Processing and gridding spatial data using Green's functions

Correct structural index in Euler deconvolution via base-level estimates

Ellipsoids (v1.0): 3D Magnetic modelling of ellipsoidal bodies

Fast iterative equivalent-layer technique for gravity data processing: A method grounded on excess mass constraint

The monogenic signal of potential-field data: A Python implementation

Step-by-step NMO correction

Fast non-linear gravity inversion in spherical coordinates with application to the South American Moho

Tesseroids: forward modeling gravitational fields in spherical coordinates

Estimating the magnetization distribution within rectangular rock samples

How two gravity-gradient inversion methods can be used to reveal different geologic features of ore deposit — A case study from the Quadrilátero Ferrífero (Brazil)

Edge detection of potential-field sources using scale-space monogenic signal: Fundamental principles

Estimation of the total magnetization direction of approximately spherical bodies

Imaging iron ore from the Quadrilátero Ferrífero (Brazil) using geophysical inversion and drill hole data

Geophysical tutorial: Euler deconvolution of potential-field data

Estimating the nature and the horizontal and vertical positions of 3D magnetic sources using Euler deconvolution

3-D radial gravity gradient inversion

Polynomial equivalent layer

Robust 3D gravity gradient inversion by planting anomalous densities

Source geometry estimation using the mass excess criterion to constrain 3-D radial inversion of gravity data