Add to ORKGTHE gravity disturbing potential T can be calculated by gravity gradient componentsTij(Txx, Txy, Txz, Tyy, Tyz, Tzz) separately. First calculate the disturbing potential by each FTG components, then the consistency of the results are compared. For the representation of regional gravity data, Fourier Series representation which can express the solution of th
Gravity gradients are an effective method for delineating the extent of subsurface density anomalies...
Summary. This paper introduces a new matrix computationai approach to the local determination of gra...
Representation of data on the sphere is conventionally done using spherical harmonics. Making use of...
Accurate and highly precise gravity gradient data are an important component of, for example, gravit...
High order, high precision geopotential models have broad application. Computing gravity and gravity...
Gravity gradiometry measurement allows imaging of anomalous sources in more detail than conventional...
<p>In the Earth gravity-field model, potential coefficients are projections of the Earth gravitation...
Traditionally, algorithms involving Fast Fourier Transforms (FFT) are used to calculate gradients fr...
Four widely used algorithms for the computation of the Earth's gravitational potential and its first...
The Normalized Full Gradient (NFG) method which was put forward about 50 years ago has been used for...
We propose a methodology for local gravity field modelling from gravity data using spherical radial ...
We present a new method for gravity data inversion for the linear problem (reconstruction of density...
As a first approximation the Earth is a sphere; as a second approximation it may be considered an el...
We modeled the effect of the deformation of a Density Gradient Zone (DGZ) on a local gravity field u...
The purpose of this paper is the canonical connection of classical global gravity field determinatio...
Gravity gradients are an effective method for delineating the extent of subsurface density anomalies...
Summary. This paper introduces a new matrix computationai approach to the local determination of gra...
Representation of data on the sphere is conventionally done using spherical harmonics. Making use of...
Accurate and highly precise gravity gradient data are an important component of, for example, gravit...
High order, high precision geopotential models have broad application. Computing gravity and gravity...
Gravity gradiometry measurement allows imaging of anomalous sources in more detail than conventional...
<p>In the Earth gravity-field model, potential coefficients are projections of the Earth gravitation...
Traditionally, algorithms involving Fast Fourier Transforms (FFT) are used to calculate gradients fr...
Four widely used algorithms for the computation of the Earth's gravitational potential and its first...
The Normalized Full Gradient (NFG) method which was put forward about 50 years ago has been used for...
We propose a methodology for local gravity field modelling from gravity data using spherical radial ...
We present a new method for gravity data inversion for the linear problem (reconstruction of density...
As a first approximation the Earth is a sphere; as a second approximation it may be considered an el...
We modeled the effect of the deformation of a Density Gradient Zone (DGZ) on a local gravity field u...
The purpose of this paper is the canonical connection of classical global gravity field determinatio...
Gravity gradients are an effective method for delineating the extent of subsurface density anomalies...
Summary. This paper introduces a new matrix computationai approach to the local determination of gra...
Representation of data on the sphere is conventionally done using spherical harmonics. Making use of...