Adigital two – dimensional elastic model was built to investigate the recent tectonic forces and stresses in Central Europe. Stresses and deformations were calculated using finite element method. The structure of model includes geologically defined features: 32 tectonic blocks, 16 fault zones and 12 boundary segments. The loads were implemented in two ways: as the external boundary forces and the correction due to differences in gravitational potential energy. The calculated stress directions and regimes were satisfactorily matched to the complex stress pattern in Central Europe provided by the World Stress Map Database. Modelling permits evaluation of tectonic forces acting in the collision zone between Africa and Arabia on one side, and E...
We use a thin-sheet approach for a viscous lithosphere to investigate the effects induced by the Alp...
The stress state in the earth crust is an important quantity for many scientific and technical quest...
After a rapid multiphase evolution and a transition from passive to active rifting during late Early...
2-D elastic finite element models of the recent stress field of Central Europe are built to evaluate...
We present the results of finite element modelling of the recent stress field in the Pannonian basin...
We present the results of finite element modelling of the recent stress field in the Pannonian basin...
An attempt is made to quantify the implications of the hypothesis that the recent-present deformatio...
The large-scale crustal deformations observed in the Central European Basin System (CEBS) are the r...
An attempt is made to quantify the implications of the hypothesis that the recent-present deformatio...
The present-day stress field in the Earth's crust is important and provides insights into mechanisms...
The highly heterogeneous strain field indicated by neotectonic and seismological data in the central...
Tectonic studies show that intraplate Europe is more active than might be expected from its tectonic...
We use a thin sheet approach to investigate the effects induced by the Alpine collision on the defor...
Predictions from dynamic modelling of the lithospheric deformation are presented for Northern Europe...
The results obtained from a suite of spherical, thin sheet, finite element model calculations on the...
We use a thin-sheet approach for a viscous lithosphere to investigate the effects induced by the Alp...
The stress state in the earth crust is an important quantity for many scientific and technical quest...
After a rapid multiphase evolution and a transition from passive to active rifting during late Early...
2-D elastic finite element models of the recent stress field of Central Europe are built to evaluate...
We present the results of finite element modelling of the recent stress field in the Pannonian basin...
We present the results of finite element modelling of the recent stress field in the Pannonian basin...
An attempt is made to quantify the implications of the hypothesis that the recent-present deformatio...
The large-scale crustal deformations observed in the Central European Basin System (CEBS) are the r...
An attempt is made to quantify the implications of the hypothesis that the recent-present deformatio...
The present-day stress field in the Earth's crust is important and provides insights into mechanisms...
The highly heterogeneous strain field indicated by neotectonic and seismological data in the central...
Tectonic studies show that intraplate Europe is more active than might be expected from its tectonic...
We use a thin sheet approach to investigate the effects induced by the Alpine collision on the defor...
Predictions from dynamic modelling of the lithospheric deformation are presented for Northern Europe...
The results obtained from a suite of spherical, thin sheet, finite element model calculations on the...
We use a thin-sheet approach for a viscous lithosphere to investigate the effects induced by the Alp...
The stress state in the earth crust is an important quantity for many scientific and technical quest...
After a rapid multiphase evolution and a transition from passive to active rifting during late Early...