<p>This work represents an improvement of the methodology applied in the geological study of a napped structure by approaching the fault system and the formations in a 3D volumetric space. From a geological point of view, the studied area contains two thrust nappes: the Hășmaș Nappe, which is a gravitational nappe and the Bukovinian Nappe, which is an overthrust nappe. By combining data obtained from field measurements with the bibliographic support, we performed an overview of the study area. The 3D geological model has been achieved by the interpretation and drawing of 54 geological cross sections based on preexisting geological maps and accumulated field knowledge, using GSI3D and Move3D software. By using the model, one can extract info...
The studied area, located in the south-western part of the Gorce Mountains, is built of flysch depos...
The use of three-dimensional (3D) modelling and visualization techniques is an effective tool that h...
In order to improve the railway connection between Austria and Italy, a base tunnel, extending from ...
Reconstruction of the structure of the upper part of the sedimentary cover (Hercynian and Alpine str...
A velocity model of the upper crust (maximum depth 10-15 km) of the earthquake-prone Vrancea area (R...
In this report, one can find a summary of the results and the methods used in a BSc-thesis, with as ...
The study area is located in the northern part of the Tatra Mts. The 3D geological model of the numm...
To investigate the geometrical relationships between folding and thrust faulting, we built a 3D geol...
This paper presents an approach to reconstruct geological structures in three dimensions using and h...
Abstract: The completion of the Bouguer gravity map for the Romanian territory, as well as the calcu...
In this paper we explore the possibility of reconstructing the topography of a confined area which i...
Tectonic Problems in the Western Part of Pădurea Craiului Massif (Apuseni Mts.). Pădurea Craiului Ma...
Detailed mapping and 3D structural modeling of the area around St. Nazaire le Desert, in the French ...
Paleostress calculation and analysis of mesoscopic structures are integrated with depth interpreted ...
It has been widely documented that the depth of foredeeps does not always reflect the topography of ...
The studied area, located in the south-western part of the Gorce Mountains, is built of flysch depos...
The use of three-dimensional (3D) modelling and visualization techniques is an effective tool that h...
In order to improve the railway connection between Austria and Italy, a base tunnel, extending from ...
Reconstruction of the structure of the upper part of the sedimentary cover (Hercynian and Alpine str...
A velocity model of the upper crust (maximum depth 10-15 km) of the earthquake-prone Vrancea area (R...
In this report, one can find a summary of the results and the methods used in a BSc-thesis, with as ...
The study area is located in the northern part of the Tatra Mts. The 3D geological model of the numm...
To investigate the geometrical relationships between folding and thrust faulting, we built a 3D geol...
This paper presents an approach to reconstruct geological structures in three dimensions using and h...
Abstract: The completion of the Bouguer gravity map for the Romanian territory, as well as the calcu...
In this paper we explore the possibility of reconstructing the topography of a confined area which i...
Tectonic Problems in the Western Part of Pădurea Craiului Massif (Apuseni Mts.). Pădurea Craiului Ma...
Detailed mapping and 3D structural modeling of the area around St. Nazaire le Desert, in the French ...
Paleostress calculation and analysis of mesoscopic structures are integrated with depth interpreted ...
It has been widely documented that the depth of foredeeps does not always reflect the topography of ...
The studied area, located in the south-western part of the Gorce Mountains, is built of flysch depos...
The use of three-dimensional (3D) modelling and visualization techniques is an effective tool that h...
In order to improve the railway connection between Austria and Italy, a base tunnel, extending from ...