In this paper we will explore the performances of the joint inversion, through the Euler reduced equations, of more ridges converging to the same source (Euler deconvolution for a multiridge set). The application to the total field due to synthetic sources demonstrate the improvements in the source parameters estimation with respect to the single ridge inversion even in the case of the simultaneous estimation of two parameters. The method yields a good clustering of the solutions and could not require any acceptance criterion or a-posteriori processing
We present a method for combining seismic deconvolution and geostatistical interpolation. Both probl...
Abstract. It is difficult to obtain high-resolution images by 3D gravity inversion, because the prob...
In full waveform inversion (FWI) we need to know the seismic source signature. In practice this is g...
In this paper we will explore the performances of the joint inversion, through the Euler reduced equ...
Potential field interpretation can be carried out using multiscale methods. This class of methods an...
A new method based on 3D multiridge analysis of potential fields assumes a 3D subset in the harmonic...
A new method based on 3D multiridge analysis of potential fields assumes a 3D subset in the harmonic...
The Euler homogeneity relation expresses how a ho-mogeneous function transforms under scaling. When ...
<p>Poster (Parts 1 and 2) presented at EAGE 2014 - 76th EAGE Conference & Exhibition 2014 (Amsterdam...
<div>Euler deconvolution is a technique based anomaly measurements, its derivatives and structural i...
We generalized the Euler deconvolution method to a joint scheme, which consists of locating the hori...
Conventional Euler deconvolution is widely used for interpreting profile, grid, and ungridded potent...
The voluminous gravity and magnetic datasets demand automatic interpretation techniques like Naudy, ...
In this tutorial we present a historical overview of the evolution of Euler deconvolution method con...
The conventional Euler deconvolution has 5 unknown parameters to be solve which are the location of ...
We present a method for combining seismic deconvolution and geostatistical interpolation. Both probl...
Abstract. It is difficult to obtain high-resolution images by 3D gravity inversion, because the prob...
In full waveform inversion (FWI) we need to know the seismic source signature. In practice this is g...
In this paper we will explore the performances of the joint inversion, through the Euler reduced equ...
Potential field interpretation can be carried out using multiscale methods. This class of methods an...
A new method based on 3D multiridge analysis of potential fields assumes a 3D subset in the harmonic...
A new method based on 3D multiridge analysis of potential fields assumes a 3D subset in the harmonic...
The Euler homogeneity relation expresses how a ho-mogeneous function transforms under scaling. When ...
<p>Poster (Parts 1 and 2) presented at EAGE 2014 - 76th EAGE Conference & Exhibition 2014 (Amsterdam...
<div>Euler deconvolution is a technique based anomaly measurements, its derivatives and structural i...
We generalized the Euler deconvolution method to a joint scheme, which consists of locating the hori...
Conventional Euler deconvolution is widely used for interpreting profile, grid, and ungridded potent...
The voluminous gravity and magnetic datasets demand automatic interpretation techniques like Naudy, ...
In this tutorial we present a historical overview of the evolution of Euler deconvolution method con...
The conventional Euler deconvolution has 5 unknown parameters to be solve which are the location of ...
We present a method for combining seismic deconvolution and geostatistical interpolation. Both probl...
Abstract. It is difficult to obtain high-resolution images by 3D gravity inversion, because the prob...
In full waveform inversion (FWI) we need to know the seismic source signature. In practice this is g...