AB: Inversion of large-scale potential-field anomalies, aimed at determining density or magnetization, is usually made in the Fourier domain. The commonly adopted geometry is based on a layer of constant thickness, characterized by a bottom surface at a fixed distance from the top surface.....UnpublishedFort Lauderdale, Florida (USA)2.6. TTC - Laboratorio di gravimetria, magnetismo ed elettromagnetismo in aree attiveope
It is shown how a series of Fourier transforms can be used to calculate the magnetic or gravitationa...
We present an algorithm for the linear inversion of 2D surface magnetic data to obtain 3D models of ...
A careful management of the data errors in potential field inversion is crucial for obtaining reliab...
AB: Inversion of large-scale potential-field anomalies, aimed at determining density or magnetizatio...
Inversion of large-scale potential-field anomalies, aimed at determining density or magnetization, i...
Inversion of large-scale potential-field anomalies, aimed at determining density or magnetization, i...
Inversion of large-scale potential-field anomalies usually proceeds in the Fourier domain, where a l...
We show an algorithm for the linear inversion of 2D surface magnetic data to obtain 3D models of the...
This thesis deals with the inversion of potential field data. Theoretical aspects and applications i...
The study of gravity and magnetism has a long history in Earth sciences and continues to play an imp...
The purpose of this work is to introduce a new inversion method of potential field, based on a 3D mo...
This thesis deals with the inversion of potential field data. Theoretical aspects and applications ...
International audienceThe use of potential field methods for geophysical exploration purposes is now...
The aim of this thesis is to implement an integrated approach of potential fields data analysis, whi...
Self-Potential data have been widely used in numerous applications. The interpretation of SP data fr...
It is shown how a series of Fourier transforms can be used to calculate the magnetic or gravitationa...
We present an algorithm for the linear inversion of 2D surface magnetic data to obtain 3D models of ...
A careful management of the data errors in potential field inversion is crucial for obtaining reliab...
AB: Inversion of large-scale potential-field anomalies, aimed at determining density or magnetizatio...
Inversion of large-scale potential-field anomalies, aimed at determining density or magnetization, i...
Inversion of large-scale potential-field anomalies, aimed at determining density or magnetization, i...
Inversion of large-scale potential-field anomalies usually proceeds in the Fourier domain, where a l...
We show an algorithm for the linear inversion of 2D surface magnetic data to obtain 3D models of the...
This thesis deals with the inversion of potential field data. Theoretical aspects and applications i...
The study of gravity and magnetism has a long history in Earth sciences and continues to play an imp...
The purpose of this work is to introduce a new inversion method of potential field, based on a 3D mo...
This thesis deals with the inversion of potential field data. Theoretical aspects and applications ...
International audienceThe use of potential field methods for geophysical exploration purposes is now...
The aim of this thesis is to implement an integrated approach of potential fields data analysis, whi...
Self-Potential data have been widely used in numerous applications. The interpretation of SP data fr...
It is shown how a series of Fourier transforms can be used to calculate the magnetic or gravitationa...
We present an algorithm for the linear inversion of 2D surface magnetic data to obtain 3D models of ...
A careful management of the data errors in potential field inversion is crucial for obtaining reliab...