All Stories

  1. Efficient equivalent-layer technique for processing irregularly spaced magnetic data on uneven surfaces
  2. Convolutional equivalent layer for magnetic data processing
  3. Magnetic amplitude inversion for depth-to-basement and apparent magnetization-intensity estimates
  4. Generalized positivity constraint on magnetic equivalent layers
  5. Convolutional equivalent layer for gravity data processing
  6. Scanning Magnetic Microscope Using a Gradiometric Configuration for Characterization of Rock Samples
  7. Isostatic constraint for 2D non-linear gravity inversion on rifted margins
  8. Amplitude of the magnetic anomaly vector for interpretation at low latitudes
  9. Equivalent layer technique for estimating magnetization direction
  10. Estimative of gravity-gradient tensor components via fast iterative equivalent-layer technique
  11. Radial magnetic inversion to retrieve the geometry of 3D sources
  12. Characterizing Complex Mineral Structures in Thin Sections of Geological Samples with a Scanning Hall Effect Microscope
  13. Ellipsoids (v1.0): 3-D magnetic modelling of ellipsoidal bodies
  14. Fast iterative equivalent-layer technique for gravity data processing: A method grounded on excess mass constraint
  15. Estimating the magnetization distribution within rectangular rock samples
  16. Estimation of the total magnetization direction of approximately spherical bodies
  17. Geophysical tutorial: Euler deconvolution of potential-field data
  18. Estimating the nature and the horizontal and vertical positions of 3D magnetic sources using Euler deconvolution
  19. 3-D radial gravity gradient inversion
  20. Estimação da geometria de corpos 3D via inversão de dados de gradiometria gravimétrica
  21. Polynomial equivalent layer
  22. Polynomial equivalent layer
  23. Source geometry estimation using the mass excess criterion to constrain 3-D radial inversion of gravity data
  24. Estimação da geometria de corpos 3D via inversão gravimétrica radial e massa anômala
  25. Radial gravity inversion constrained by total anomalous mass excess for retrieving 3D bodies