All Stories

  1. Using gravity-data uncertainties in forward modeling to estimate uncertainties in model parameters: a case history in estimating the dip and the dip uncertainty of the Porcupine Destor Fault
  2. Geophysical transects in the Abitibi greenstone belt of Canada from the mineral-exploration-oriented Metal Earth project
  3. 3D generalized spherical multifocusing seismic imaging
  4. Open-source software for two-dimensional Fourier processing of gridded magnetic data
  5. How magnetic susceptibilities measured on outcrops can be used for modelling (and constraining inversions of) aeromagnetic data
  6. Forward modeling and 3D inversion of electromagnetic data collected over the McArthur River uranium deposit in the Athabasca Basin, Canada
  7. Active and Passive Seismic Imaging of the Central Abitibi Greenstone Belt, Larder Lake, Ontario
  8. Transformation of magnetic data to the pole and vertical dip and a related apparent susceptibility transform: Exact and approximate approaches
  9. Estimating the parameters of simple models from two-component on-time airborne electromagnetic data
  10. Convolutional neural networks applied to the interpretation of lineaments in aeromagnetic data
  11. Active and passive seismic imaging of the central Abitibi greenstone belt, Larder Lake, Ontario
  12. Multiple-order moments of the transient electromagnetic response of a one-dimensional earth with finite conductance – the Gaussian variation applied to a field example
  13. On Archean craton growth and stabilisation: Insights from lithospheric resistivity structure of the Superior Province
  14. Multiple-order moments of the transient electromagnetic response of a one-dimensional earth with finite conductance – theory
  15. On the time decay constant of AEM systems: a semi-heuristic algorithm to validate calculations.
  16. A new method for interpolating linear features in aeromagnetic data
  17. Resistivity and anisotropy as a proxy for structural complexity
  18. An airborne EM system for nickel sulphide exploration
  19. The impact of magnetic viscosity on time-domain electromagnetic data from iron oxide minerals embedded in rocks at Opemiska, Québec, Canada
  20. Inductive electromagnetic data interpretation using a 3D distribution of 3D magnetic or electric dipoles
  21. Modelling and straight-ray tomographic imaging studies of cross-hole radio-frequency electromagnetic data for mineral exploration
  22. Using constrained inversion of gravity and magnetic field to produce a 3D litho-prediction model
  23. Approximate semianalytical solutions for the electromagnetic response of a dipping-sphere interacting with conductive overburden
  24. The effect of dielectric permittivity on the fields radiated from a radio-frequency electric dipole in a homogeneous whole space
  25. Combining spatial components and Hilbert transforms to interpret ground-time-domain electromagnetic data
  26. A multiple transmitter and receiver electromagnetic system for improved target detection
  27. Clustering of downhole physical property measurements at the Victoria property, Sudbury for the purpose of extracting lithological information
  28. Regional 3D geophysical investigation of the Sudbury Structure
  29. Introduction to special section: Mining and minerals exploration interpretation
  30. A procedure for collecting electromagnetic data using multiple transmitters and receivers capable of deep and focused exploration
  31. Robust conductance estimates from spatial and temporal derivatives of borehole electromagnetic data
  32. Mapping lateral changes in conductance of a thin sheet using time-domain inductive electromagnetic data
  33. Using spatial derivatives of electromagnetic data to map lateral conductance variations in thin-sheet models: Applications over mine tailings ponds
  34. Qualitative geophysical interpretation of the Sudbury Structure
  35. Electromagnetic Induction Methods in Mining Geophysics from 2008 to 2012
  36. Using combinations of spatial gradients to improve the detectability of buried conductors below or within conductive material
  37. Precision requirements for specifying transmitter waveforms used for modelling the off-time electromagnetic response
  38. Qualitative geophysical interpretation of the Sudbury structure
  39. Using spatial gradients of electromagnetic data to map lateral variations in mine tailings
  40. A grid implementation of the SLUTH algorithm for visualising the depth and structural index of magnetic sources
  41. How to make better use of physical properties in mineral exploration: The exploration site measurement
  42. Metalliferous mining geophysics— State of the art after a decade in the new millennium
  43. Mapping laterally varying conductance using EM gradients over dry tailings ponds
  44. A comparison of airborne electromagnetic data with ground resistivity data over the Midwest deposit in the Athabasca basin
  45. Automation of the SLUTH method: a novel approach to airborne magnetic data interpretation
  46. Detection of alteration at the Millennium uranium deposit in the Athabasca Basin: a comparison of data from two airborne electromagnetic systems with ground resistivity data
  47. Combined airborne time-domain electromagnetics and power-line field survey
  48. Sferics noise reduction in time-domain electromagnetic systems: application to MegaTEMIIsignal enhancement
  49. Sensitivity cross-sections in airborne electromagnetic methods using discrete conductors
  50. Application of Occam's inversion to airborne time-domain electromagnetics
  51. Case histories illustrating the characteristics of the HeliGEOTEM system
  52. Advances in airborne geophysical systems for ordnance mapping and detection
  53. Interpretation of magnetic data using tilt-angle derivatives
  54. Mapping tailings around mine sites with reverse polarity airborne transient EM data
  55. Geological mapping with power line fields measured with MEGATEM data
  56. Tilt-depth method: A simple depth estimation method using first-order magnetic derivatives
  57. Source location using total-field homogeneity: Introducing the SLUTH method for depth estimation
  58. A discrete conductor transformation of airborne electromagnetic data
  59. Generalized magnetic tilt‐Euler deconvolution
  60. Combining airborne electromagnetic data from alternating flight directions to form a virtual symmetric array
  61. Airborne EM measurements over the Shea Creek uranium prospect, Saskatchewan, Canada
  62. A discrete conductor transformation of airborne electromagnetic data
  63. An analysis of geophysical and geological data from the Iso/New Insco test site, Quebec, Canada
  64. Geophysical Case Study of the Iso and New Insco Deposits, Quebec, Canada, Part I: Data Comparison and Analysis
  65. Geophysical Case Study of the Iso and New Insco Deposits, Quebec, Canada, Part II: Modeling and Interpretation
  66. Quantifying the Effects That Changes in Transmitter-Receiver Geometry Have on the Capability of an Airborne Electromagnetic Survey System to Detect Good Conductors
  67. Interpolation and gridding of aliased geophysical data using constrained anisotropic diffusion to enhance trends
  68. An enhanced method for source parameter imaging of magnetic data collected for mineral exploration
  69. Imaging depth, structure, and susceptibility from magnetic data: The advanced source-parameter imaging method
  70. Interpretation of magnetic data using an enhanced local wavenumber (ELW) method
  71. Gridding aeromagnetic data using longitudinal and transverse horizontal gradients with the minimum curvature operator
  72. Approximate apparent conductance (or conductivity) from the realizable moments of the impulse response
  73. Depth and structural index from normalized local wavenumber of 2D magnetic anomalies
  74. Using realizable moments of the impulse response to estimate the approximate apparent conductance or apparent conductivity of the ground
  75. Interpolation and gridding of aliased geophysical data using constrained anisotropic diffusion to enhance trends
  76. Using airborne EM surveys to investigate the hydrogeology of an area near Nyborg, Denmark
  77. Combining airborne electromagnetic data from alternate flight directions to improve data interpretability: the virtual symmetric array
  78. Using a non-integer moment of the impulse response to estimate the half-space conductivity
  79. To “The moments of the impulse response: A new paradigm for the interpretation of transient electromagnetic data” (Richard S. Smith and Terry J. Lee, GEOPHYSICS, 67, 1095–1103).
  80. The moments of the impulse response of a transient electromagnetic decay
  81. A multimodel method for depth estimation from magnetic data
  82. Using the moments of a thick layer to map conductance and conductivity from airborne electromagnetic data
  83. The moments of the impulse response, a new paradigm for the interpretation of transient electromagnetic data
  84. A comparison of data from airborne, semi‐airborne, and ground electromagnetic systems
  85. On removing the primary field from fixed-wing time-domain airborne electromagnetic data: some consequences for quantitative modelling, estimating bird position and detecting perfect conductors
  86. Using an induction coil sensor to indirectly measure theB-field response in the bandwidth of the transient electromagnetic method
  87. The realizable resistive limit: A new concept for mapping geological features spanning a broad range of conductances
  88. Robust estimation of the band‐limited inductive‐limit response from impulse‐response TEM measurements taken during the transmitter switch‐off and the transmitter off‐time: Theory and an example from Voisey’s Bay, Labrador, Canada
  89. An experiment to compare airborne, semi‐airborne and ground electromagnetic systems
  90. Model‐independent depth estimation with the SPI™ method
  91. iSPI TM — the improved source parameter imaging method
  92. Automatic conversion of magnetic data to depth, dip, and susceptibility contrast using the SPI (TM) method
  93. A special circumstance of airborne induced‐polarization measurements
  94. Application of a modified GEOTEM® system to reconnaissance exploration for kimberlites in the Point Lake area, NWT, Canada
  95. The usefulness of multicomponent, time‐domain airborne electromagnetic measurements
  96. Geology from geophysics; or, converting magnetic data to depth, dip, and susceptibility contrast using the source parameter imaging (SPITM) method
  97. An automatic technique for presentation of coincident‐loop, impulse‐response, transient, electromagnetic data
  98. Conductivity‐depth imaging of airborne electromagnetic step‐response data
  99. Response by Richard Smith to the authors’ reply
  100. On: “Induced‐polarization effects in time‐domain electromagnetic measurements” by M. F. Flis, G. A. Newman, and G. W. Hohmann (GEOPHYSICS, 54, 514–523, April 1989).
  101. Field examples of negative coincident‐loop transient electromagnetic responses modeled with polarizable half‐planes
  102. Inductive interaction between polarizable conductors: An explanation of a negative coincident‐loop transient electromagnetic response
  103. Electromagnetic induction in an inhomogeneous conductive thin sheet