The Poisson's equation expresses a linear relationship between the gravity and magnetic potentials arising from a body with uniform density and magnetization contrast. The equation was extended to multi body case by repeatedly applying it within a small uniform body called the moving window. The moving-window Poisson's (MWP) analysis technique was proposed by Chandler et al. (1981) to apply to general complex structures. The correlation coefficient between the total magnetic intensity anomaly reduced to the pole and vertical derivative of the gravity anomaly, and the magnetization-to-density ratio were obtained by the MWP analysis. We investigated the profiles of these parameters for synthetic multi density and magnetic intensity structures...
We show a set of forward model equations in the Fourier domain for calculating the 3-D gravity and m...
It is shown how a series of Fourier transforms can be used to calculate the magnetic or gravitationa...
A new approach to the interpretation of magnetic anomalies generated by geological structures resemb...
Vector field formulation based on the Poisson theorem allows an automatic determination of rock phys...
Gravitational and magnetic anomalies of an arbitrary target body are linked through Poisson's differ...
Summary. Correlation of gravity and magnetic anomalies combined with other geological and geophysica...
Magnetic susceptibility has been extensively used to determine the magnetic properties of rocks for ...
A simple numerical technique that permits the determination of the magnetization of a two dimentiona...
Poisson's theorem relates linearly the derivative of the gravity potential (taken along the total ma...
Geophysical modelling can take advantage of combining more geophysical data with the aim of decreasi...
Internal correspondence uses Poisson's Theorem in a moving-window linear regression analysis between...
A simple numerical technique that permits the determination of themagnetization of a two dimentional...
Within the scope of this paper, Walsh transform was applied to the total magnetic field and gravity ...
This research deals with the processing and analyzing of magnetic and gravitational data for an area...
We show a set of forward model equations in the Fourier domain for calculating the 3D gravity and m...
We show a set of forward model equations in the Fourier domain for calculating the 3-D gravity and m...
It is shown how a series of Fourier transforms can be used to calculate the magnetic or gravitationa...
A new approach to the interpretation of magnetic anomalies generated by geological structures resemb...
Vector field formulation based on the Poisson theorem allows an automatic determination of rock phys...
Gravitational and magnetic anomalies of an arbitrary target body are linked through Poisson's differ...
Summary. Correlation of gravity and magnetic anomalies combined with other geological and geophysica...
Magnetic susceptibility has been extensively used to determine the magnetic properties of rocks for ...
A simple numerical technique that permits the determination of the magnetization of a two dimentiona...
Poisson's theorem relates linearly the derivative of the gravity potential (taken along the total ma...
Geophysical modelling can take advantage of combining more geophysical data with the aim of decreasi...
Internal correspondence uses Poisson's Theorem in a moving-window linear regression analysis between...
A simple numerical technique that permits the determination of themagnetization of a two dimentional...
Within the scope of this paper, Walsh transform was applied to the total magnetic field and gravity ...
This research deals with the processing and analyzing of magnetic and gravitational data for an area...
We show a set of forward model equations in the Fourier domain for calculating the 3D gravity and m...
We show a set of forward model equations in the Fourier domain for calculating the 3-D gravity and m...
It is shown how a series of Fourier transforms can be used to calculate the magnetic or gravitationa...
A new approach to the interpretation of magnetic anomalies generated by geological structures resemb...