International audienceWhen too few field measurements are available for the geological modeling of complex folded structures, the results of implicit methods typically exhibit an unsatisfactory bubbly aspect. However, in such cases, anisotropy data are often readily available but not fully exploited. Among them, fold axis data are a straightforward indicator of this local anisotropy direction. Focusing on the so-called potential field method, this work aims to evaluate the effect of the incorporation of such data into the modeling process. Given locally sampled fold axis data, this paper proposes to use the second-order derivatives of the scalar field in addition to the existing first-order ones. The mathematical foundation of the approach ...
Recently, there has been a dramatic increase in the use of scale invariance in the study of geophysi...
this paper we show some of the effects that appear in magnetotelluric measurements over 2-D anisotro...
Several landforms are known to exhibit topographic anisotropy, defined as a directional inequality i...
Les méthodes de modélisation géologique 3D ont pour but de construire des modèles numériques cohéren...
International audienceGeological structures, such as complex folds, fluvial channels or ore-veins, u...
International audienceA recent method for modeling folds uses a fold frame with coordinates based on...
Three-dimensional geological modelling methods aim at building relevant and coherent underground num...
Folds present a challenge for 3D modelling because the information associated with the geometry of t...
International audienceThree-dimensional structural modeling is gaining importance for a broad range ...
International audienceSedimentary units generally present anisotropy in their hydraulic properties, ...
International audienceStructural sampling in the field is usually dependent of the mapping path chos...
By applying differential geometry to analogue models developed by Grujic et al. (2002), we demonstra...
Most 3D geological modelling tools were designed for the needs of the oil industry and are not suite...
The maximum, minimum, Gaussian, and mean curvatures of a folded bedding surface are calculated from ...
Geological surveying is a common practice performed by geologists nowadays. Determining layer orient...
Recently, there has been a dramatic increase in the use of scale invariance in the study of geophysi...
this paper we show some of the effects that appear in magnetotelluric measurements over 2-D anisotro...
Several landforms are known to exhibit topographic anisotropy, defined as a directional inequality i...
Les méthodes de modélisation géologique 3D ont pour but de construire des modèles numériques cohéren...
International audienceGeological structures, such as complex folds, fluvial channels or ore-veins, u...
International audienceA recent method for modeling folds uses a fold frame with coordinates based on...
Three-dimensional geological modelling methods aim at building relevant and coherent underground num...
Folds present a challenge for 3D modelling because the information associated with the geometry of t...
International audienceThree-dimensional structural modeling is gaining importance for a broad range ...
International audienceSedimentary units generally present anisotropy in their hydraulic properties, ...
International audienceStructural sampling in the field is usually dependent of the mapping path chos...
By applying differential geometry to analogue models developed by Grujic et al. (2002), we demonstra...
Most 3D geological modelling tools were designed for the needs of the oil industry and are not suite...
The maximum, minimum, Gaussian, and mean curvatures of a folded bedding surface are calculated from ...
Geological surveying is a common practice performed by geologists nowadays. Determining layer orient...
Recently, there has been a dramatic increase in the use of scale invariance in the study of geophysi...
this paper we show some of the effects that appear in magnetotelluric measurements over 2-D anisotro...
Several landforms are known to exhibit topographic anisotropy, defined as a directional inequality i...