The separation of the effects of deep-seated sources of potential fields from those of shallower ones is a frequent requirement when interpreting magnetic or gravity fields. A common procedure is estimating the regional, long wavelength, component of the field by analysing the data over an area larger than that of the local feature of interest. The local components are found by subtracting the estimated regional from the observed data. These approaches may have difficulties in their application, as the dataset over large areas may not be available and other local anomalies, in the enlarged area, may prevent a reliable estimate of the regional field. We present an alternative and simple approach to the regional-residual separatio...
This chapter is aimed at demonstrating how the second vertical derivative method is been applied to ...
Abstract: Two dimensional Fourier transform can be used for the upward continuation of gravity or ma...
A new imaging method is developed to estimate the depth to the sources of potential fields, independ...
Economic exploitation of mineral resources, especially in underdeveloped mountainous areas, requires...
The second vertical derivative of magnetic fields is commonly used for resolution of anomalies in gr...
This paper presents quantitative application of Least-Square Polynomial fitting method in regional-r...
Two key areas in aeromagnetic interpretation are discussed. Firstly, the problem of separating geolo...
Resolving regional and residual components arising out of deeper and shallower sources in observed B...
Conventional reductions of gravity and mag-netic data do not lead to values that are ef-fectively on...
Abstract: A new method for regional-residual magnetic field data separation, in wavelet domain, is s...
Imaging of potential fields yields a fast 3D representation of the source distribution of potential ...
Traditionally, algorithms involving Fast Fourier Transforms (FFT) are used to calculate gradients fr...
THE gravity disturbing potential T can be calculated by gravity gradient componentsTij(Txx, Txy, Txz...
Downward continuation is a useful transformation, mainly used to enhance measured gravity or magneti...
In this paper we present a method to separate anomalies corresponding to bodies at different depths,...
This chapter is aimed at demonstrating how the second vertical derivative method is been applied to ...
Abstract: Two dimensional Fourier transform can be used for the upward continuation of gravity or ma...
A new imaging method is developed to estimate the depth to the sources of potential fields, independ...
Economic exploitation of mineral resources, especially in underdeveloped mountainous areas, requires...
The second vertical derivative of magnetic fields is commonly used for resolution of anomalies in gr...
This paper presents quantitative application of Least-Square Polynomial fitting method in regional-r...
Two key areas in aeromagnetic interpretation are discussed. Firstly, the problem of separating geolo...
Resolving regional and residual components arising out of deeper and shallower sources in observed B...
Conventional reductions of gravity and mag-netic data do not lead to values that are ef-fectively on...
Abstract: A new method for regional-residual magnetic field data separation, in wavelet domain, is s...
Imaging of potential fields yields a fast 3D representation of the source distribution of potential ...
Traditionally, algorithms involving Fast Fourier Transforms (FFT) are used to calculate gradients fr...
THE gravity disturbing potential T can be calculated by gravity gradient componentsTij(Txx, Txy, Txz...
Downward continuation is a useful transformation, mainly used to enhance measured gravity or magneti...
In this paper we present a method to separate anomalies corresponding to bodies at different depths,...
This chapter is aimed at demonstrating how the second vertical derivative method is been applied to ...
Abstract: Two dimensional Fourier transform can be used for the upward continuation of gravity or ma...
A new imaging method is developed to estimate the depth to the sources of potential fields, independ...